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Srikantia, S. V.
- Report on Field Workshop on Integrated Evaluation of the Kaladgi and Bhima Basins - October 21-25, 1999
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Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 55, No 2 (2000), Pagination: 207-210Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting
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PDF Views:122
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 55, No 1 (2000), Pagination: 99-101Abstract
No Abstract.Full Text
- Bhopal '99
Abstract Views :176 |
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Authors
Affiliations
1 Geological Society of India Bangalore - 560 019, IN
1 Geological Society of India Bangalore - 560 019, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 55, No 3 (2000), Pagination: 329-330Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting, Chennai '97
Abstract Views :177 |
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Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 51, No 1 (1998), Pagination: 113-114Abstract
No Abstract.Full Text
- Geology of Pakistan (1995)
Abstract Views :141 |
PDF Views:228
Authors
Affiliations
1 Geological Society of India, Bangalore, IN
1 Geological Society of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 51, No 1 (1998), Pagination: 128-130Abstract
No Abstract.Full Text
- Neotectonic Map of China and Adjacent Seas
Abstract Views :202 |
PDF Views:138
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 51, No 6 (1998), Pagination: 833-834Abstract
No Abstract.Full Text
- Restriction on Maps - An Anachronism that Needs Removal
Abstract Views :164 |
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Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 53, No 3 (1999), Pagination: 367-371Abstract
No Abstract.Full Text
- Proceedings of the Annual General meeting
Abstract Views :180 |
PDF Views:102
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 53, No 1 (1999), Pagination: 105-107Abstract
No Abstract.Full Text
- Opening of Ocean Science and Technology Cell (OSTC) for Beach Placer Minerals in the Dept. of Earth Science, Tamil University, Thanjavur and Colloquim on Beach Placers, 5-6 December 1998
Abstract Views :175 |
PDF Views:128
Authors
Affiliations
1 Geological Society of India, IN
1 Geological Society of India, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 53, No 4 (1999), Pagination: 472-472Abstract
No Abstract.Full Text
- Simla Group - A Reclassification of the 'Chail Series' 'Jaunsar Series' and 'Simla Slates' in the Simla Himalaya
Abstract Views :234 |
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Authors
Affiliations
1 Chandigarh, IN
2 Indian Photo-Interpretation Institute, Dehradun, IN
1 Chandigarh, IN
2 Indian Photo-Interpretation Institute, Dehradun, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 12, No 3 (1971), Pagination: 234-240Abstract
The study of 'Chail Series', 'Jaunsar Series' and 'Simla Slates' in the Simla Himalaya has brought out the incongruities in the present lithostratigraphy of these formations. The Simla group, divisible into four formations, is the revised classification proposed. The Basantpur, with shale, siltstone and abundant limestone interbeds, is at the bottom of the Simla group sequence, and in the ascending order, succeeded by the Kunihar with shale and stromatolitic limestone, the Chhaosa containing flysch sediments and the Sanjauli with conglomerate and grit facies. The Simla group represents a typical geosynclinal cycle of sedimentation deposited over the Shali, Sundernagar and Mandi-Darla volcanic rocks.
- The Occurrence of Rocks of Kakara (Paleocene) Affinity in the Bakhalag-Bughar Belt, Himachal Pradesh
Abstract Views :170 |
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Authors
Affiliations
1 Chandigarh, IN
1 Chandigarh, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 11, No 2 (1970), Pagination: 185-188Abstract
No Abstract.Full Text
- The 'Jaunsar' Problem in the Himalaya - A Critical Analysis and Elucidation
Abstract Views :188 |
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Authors
Affiliations
1 98-99-100, Sector 17-C, Chandigarh-17, IN
1 98-99-100, Sector 17-C, Chandigarh-17, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 15, No 2 (1974), Pagination: 115-136Abstract
A complex association of limestones, quartzites, slates and volcanic rocks and ashes exposed In the Garhwal Himalaya was first called as 'Jaunsar System' by Oldham. Pilgrim and West adopted the name 'Jaunsar' for their Jagas Series c - a selective quartzite-slate association, and Auden variously considered his Mandhali-Chandpur-Nagthat association of diverse lithology, and the Nagth Nagthat Series of quartzite-phyllite association as 'Jaunsar'. Later workers either adopted the classification of Pilgrim and West, or of Auden, or reclassified the Chandpur-Nagthat to include crystallines and metamorphics, without much regard to the larger stratigraphic Implications of the same. This has resulted In great confusion In the stratigraphy of the Himalayas leading to conjectural correlations of formations and hypothetical interpretation of structures.
The present study has shown that the 'Jaunsars' are variously part of the Simla group of Srikantia and Sharma or are part of the sequence of the Mandhali-Chandpur-Nagthat. The recent attempt to include rock types referable to the Jutogh as part of the Chandpur-Nagthat is mainly due to the non-recognition of a thrust contact between these two which is obscured due to post-tectonic metamorphism and deformation, and hence is not an acceptable proposition.
It is now proposed to redefine the term 'Jaunsar' and to strictly restrict it to the restored sequence of Mandhali, Chandpur and Nagthat formations. The Jaunsar group as adopted now represents a typical geosynclinal type of sediments deposited on the eroded surface of the Deoban belt. It is characterised by the association of the Bhowali volcanics and the acid intrusives of the Kharasali gneiss, and is typically eugeosynclinal. Structurally it occurs as a superficial nappe over the isopic zones of the Deoban-Simla group in the southern part of the Deoban belt.
The Jaunsar group, the Simla group and the Rampur formation are considered as contemporaneous formations in the present scheme of correlation of geosynclinal sediments In the Lesser HImalaya.
- The Sundernagar Group: Its Geology, Correlation and Significance as Stratigraphically the Deepest Sediment in the Peninsular or Lesser Himalaya
Abstract Views :233 |
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Authors
Affiliations
1 Geological Survey of India, Nilofar Building, Raj Bagh, Srinagar 190008, Jammu & Kashmir, IN
1 Geological Survey of India, Nilofar Building, Raj Bagh, Srinagar 190008, Jammu & Kashmir, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 18, No 1 (1977), Pagination: 7-22Abstract
An association of quartzite, slate and basic volcanics forming the foundation of the Shali Group is designated as the Sundernagar Group. The base of this formation is not exposed and the entire edifice of the sequence, ranging from the Shali, Simla, Blaini, Infra-Krol, Krol, and the Tertiaries, is built upon this formation making it stratigraphically the deepest sediment in the Peninsular or the Lesser Himalaya.
As the history of the Sundernagar Group is closely linked with the events in the northern part of Peninsular India, a correlation is attempted with the Pre-Vindhyan groups like the Delhi, Bijawar and Gwalior. In the Lesser Himalaya, it has been found that most of the older Proterozoic carbonate belts like the Larji, Deoban, Tejam-Pithoragarh, Suparitar (Nawakot) and Baxa contain, at their base an association of quartzite, slate and volcanics. This proves the widespread extension of the Sundernagar rocks and the Mandi-Darla Volcanic episode in the Himalaya during the Delhi period.
From the present study it is postulated that the Pre-Delhi basement complex forms the basement for the entire sedimentary sequence in the Peninsular Himalaya.
- A Note on the Significance of Granite Clasts in a Diamictite of the Thango Formation (Lower Silurian) Zanskar Valley, Ladakh Himalaya
Abstract Views :201 |
PDF Views:126
Authors
Affiliations
1 Geological Survey of India, Nilofar Building, Raj Bagh, Srinagar 190008, IN
1 Geological Survey of India, Nilofar Building, Raj Bagh, Srinagar 190008, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 18, No 9 (1977), Pagination: 509-511Abstract
The presence of tourmaline bearing granite clasts in the diamictite of the Thango Formation (Lower Silurian) of the Haimanta Group, in Zanskar Valley of Ladakh, J&K State, suggests the existence of Pre-Silurian tourmaline granite in the Higher Himalaya.Full Text
- Geochemistry and Origin of Acidic Rocks from Jaspa and Rohtang, Himachal Pradesh
Abstract Views :204 |
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Authors
Affiliations
1 National Geophysical Research Institute, Hyderabad-500007, IN
1 National Geophysical Research Institute, Hyderabad-500007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 19, No 12 (1978), Pagination: 563-570Abstract
Geochemical investigations on the Jaspa granites and Rohtang gneisses from Himachal Pradesh indicate that the Rohtang gneisses are the migmatlsed/granltised products of the pre-existing metasediments and the Jaspa granite is an intrusive granite. Field relationship suggests that the Jaspa granite is a post-tectonic intrusive while the migmatisation/granltisation of the gneisses appear to be pre-and syntectonic and might have continued into the post-tectonic period.- The Kainchwa Granitic Complex of the Jutogh Belt of the Chaur Mountain Area, Simla Himalaya
Abstract Views :218 |
PDF Views:158
Authors
Affiliations
1 Nilofar Buildings, Rajbagh, Srinagar-190008, IN
2 Lucknow, IN
3 Samchi, Bhutan, IN
1 Nilofar Buildings, Rajbagh, Srinagar-190008, IN
2 Lucknow, IN
3 Samchi, Bhutan, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 19, No 4 (1978), Pagination: 169-170Abstract
The present note records the occurrence of a new granitic complex along the Kainchwa Tibba which represents the second granitic pluton besides the Chaur granitic pluton of the Jutogh belt of the Chaur mountain area. It is mainly a complex of leucogranite and gneisses.Full Text
- The Tandi Group of Lahaul-Its Geology and Relationship with the Central Himalayan Gneiss
Abstract Views :191 |
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Authors
Affiliations
1 Nilofar, Rajbagh, Srinagar-190008, IN
2 529, Sector 18B, Chandigarh, IN
1 Nilofar, Rajbagh, Srinagar-190008, IN
2 529, Sector 18B, Chandigarh, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 20, No 11 (1979), Pagination: 531-539Abstract
The Tandi Group of Lahaul area in the Himachal Higher Himalaya represents a sequence of essentially carbonate rocks. It is underlain by chlorite phyllite representing possibly metamorphosed lava flows and overlies Precambrian-Eocambrian Batal Formation of the Haimanta Group. The Tandi Group has yielded significant fossil assemblage indicating a Permian to Triassic and possibly Jurassic age. Structurally, the Tandi Group constitutes an overturned syncline with a southwest dipping axial plane. The overturned limb has thrust imbricates suggesting a direction of movement from sw to NE.
The Tandi Group represents a major Permo-Trias marine transgression from Kashmir in NW through Bhallesh and Chamba. It has no direct relationship with the Central Crystalline Gneiss which occupies stratigraphically the deepest position in the area and forms a geanticline separating the Spiti-Zanskar basin from the Kashmir-Bhallesh-Chamba- Tandi-basins.
The Tandi rocks suffered intense deformation together with the basement rocks due to its proximity to the main orographic axis. The Precambrian-Eocambrian basement rocks have vestiges of folds older than the Himalayan folds.
- Geology of Part of Central Ladakh Himalaya with Particular Reference to Indus Tectonic Zone
Abstract Views :246 |
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Authors
Affiliations
1 'Nilofar', Rajbagh, Srinagar-190008, IN
1 'Nilofar', Rajbagh, Srinagar-190008, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 21, No 11 (1980), Pagination: 523-545Abstract
In the Central Ladakh Himalaya, the Ladakh Granitic Complex with Kharbu Group, the Indus Tectonic Zone and the Spiti-Zanskar and Kashmir Precambrian Phanerozoic belts constitute the chief geological units. The Ladakh Granitic Complex comprises a heterogeneous association of granitoids, gabbroids and basic rocks. The Spiti-Zanskar and Kashmir belts comprise Precambrian-Eocambrian crystallines and Late Palaeozoic-Mesozoic sediments.The Indus Tectonic Zone, a name adopted in preference to the Indus Suture Zone consists of two parallel and almost homotaxial sedimentary belts viz., the non-ophiolitic Indus Group in the north and the ophiolitic sedimentary volcanic belt of the Sangeluma Group in the south. The Indus Group unconformably overlies the Ladakh Granitic Complex, and the Sangeluma Group tectonically overlies the former. The Indus Group is divisible into the Skinding, the Kuksho, the Maklishun and the Karit Formations in the ascending order, and the Sangeluma into the Khalsi, the Dras Volcanic, the Nindam and the Shergol Formations with ophiolite association in all the formations excepting the Nindam.
The Indus Group cycle of sedimentation comprises, shallow diamictite, flyschoid, lagoonal and molassic stages, whereas the Sangeluma comprises the platform, submarine volcanic, flyschoid and unstable shelf type sedimentation.
Tectonically, the area can be divided into: Ladakh Granitic Complex-Indus Group autochthon, the Sangeluma parautochthon, the Kuling-Lilang schuppen belt, the parautochthon of Spiti-Zanskar and Kashmir Precambrian-Phaneroxoic belts and Shilakong ophiolite nappe.
The Indus Tectonic Zone was an original mega lineament which later became a site of opening of sea and sedimentation for the Indus and the Sangeluma. A sequence of stages of sea-floor spreading subduction and closing is envisaged.
- Shilakong Ophiolite Nappe of Zanskar Mountains, Ladakh Himalaya
Abstract Views :194 |
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Authors
Affiliations
1 29, Jawaharlal Nehru Road, Calcutta 700016, IN
2 B-ll, H. Road, Lucknow 226006, IN
1 29, Jawaharlal Nehru Road, Calcutta 700016, IN
2 B-ll, H. Road, Lucknow 226006, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 22, No 5 (1981), Pagination: 227-234Abstract
The Shilakong ophiolite nappe occurs along the crest of the Zanskar Mountains in Ladakh, tectonically resting over the Mesozoic-Cenozoic sediments of the Spiti-Zanskar basin. It comprises two sub-nappe units. The lower Photang sub-nappe is made of pillow lava, basalt, volcanogenic sediments, purple chert and carbonate rocks with slivers of serpentinite. The Spong sub-nappe comprises mainly harzburgite, dunite and lherzolite in different stages of serpentinisation. The Shilakong ophiolite nappe is comparable with the Kiogar-Amlang La ophiolite nappe complex south of Kailas in South Tibet-North Kumaun region. These ophiolite nappes represent squeezed up material from the deep sea regime along the Inclus Tectonic Zone and are now obducted onto the continental zone as the highest allochthon in the Himalaya.- A Note on the Tectonic Framework and Geologic Set-Up of the Pangong-Chushul Sector, Ladakh Himalaya
Abstract Views :208 |
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Authors
Affiliations
1 29, J. L. Nehru Road, Calcutta 700 076, IN
2 Nilofar, Rajbagh, Srinagar 190 008, IN
1 29, J. L. Nehru Road, Calcutta 700 076, IN
2 Nilofar, Rajbagh, Srinagar 190 008, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 23, No 7 (1982), Pagination: 354-357Abstract
The Pangong Tso-Spanggur Tso and the Shyok-Chushul-Dungti are the two tectonic zones in the area north of the Ladakh Range. The former zone has an association of metapelites, metacarbonates and metavolcanics in a graben type basin bounded by granitoids. The latter zone comprises Orbilina limestone, argillite, lava flows and grey-purple conglomerates in another graben type basin bounded on the NE by Pangong Granitoid and on the sw by the Ladakh Granitoid belts. These, along with the Indus Tectonic zone represent NW-SE trending parallel tectonic zones in the Trans-Himalayan Zone. The Pangong Tso-Spanggur Tso appear to be part of the larger Permian basin of Tibet. The Orbiloina limestone-volcanics-conglomerates or the Shyok-Chushul Tectonic Zone are comparable with the Sangeluma belt or the Indus Tectonic Zone. These are independent zones but comtemporaneous in development.Full Text
- History of Paleozoic Salt Accumulation
Abstract Views :196 |
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Authors
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Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 23, No 9 (1982), Pagination: 465-466Abstract
No Abstract.Full Text
- Taphrohelminthopsis Circularis from Cambrian Sediments of Southeast Kashmir Valley
Abstract Views :193 |
PDF Views:136
Authors
Affiliations
1 29, J. L. Nehru Road, Calcutta, IN
1 29, J. L. Nehru Road, Calcutta, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 23, No 8 (1982), Pagination: 406-407Abstract
An ichnofossil Taphrohelminthopsis circularis Crimes et af., 1977, is being reported from the (?) Cambrian sediments exposed along the Hapatnar-Hangalpau road near Hangalpau, Anantnag district, Kashmir.Full Text
- Geotectonics
Abstract Views :172 |
PDF Views:106
Authors
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Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 23, No 10 (1982), Pagination: 518-519Abstract
No Abstract.Full Text
- Mesozoic Ammonites from the Spong Valley, Zanskar, N. W. India
Abstract Views :188 |
PDF Views:118
Authors
Affiliations
1 A.M.S.E. Wing, Geological Survey of India, Bangalore-560 004, IN
1 A.M.S.E. Wing, Geological Survey of India, Bangalore-560 004, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 23, No 12 (1982), Pagination: 624-625Abstract
No Abstract.Full Text
- Gondwana Five
Abstract Views :190 |
PDF Views:127
Authors
Affiliations
1 Geological Survey of India, AMSE Wing, IN
1 Geological Survey of India, AMSE Wing, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 24, No 6 (1983), Pagination: 321-323Abstract
No Abstract.Full Text
- Continental Endogenous Regimes
Abstract Views :195 |
PDF Views:109
Authors
Affiliations
1 Geological Survey of India, AMSE Wing, Bangalore, IN
1 Geological Survey of India, AMSE Wing, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 24, No 11 (1983), Pagination: 606-607Abstract
No Abstract.Full Text
- The Jutogh Klippe of the Simla Area of the Himachal Himalaya: Its Geology and Structural Evolution
Abstract Views :171 |
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Authors
Affiliations
1 1116, 10th Cross, Banasankari I Stage, II Block, Bangalore 560050, IN
2 529, Sector 18-B, Chandigarh 160018, IN
1 1116, 10th Cross, Banasankari I Stage, II Block, Bangalore 560050, IN
2 529, Sector 18-B, Chandigarh 160018, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 25, No 4 (1984), Pagination: 220-230Abstract
The Jutogh klippe near simla is the highest allochthon in the Himachal Himalaya. Its base is defined by the Jutogh Thrust. Five mappable lithostratigraphic formations are recognised. These are variously represented, in the ascending order, by carbonaceous phyllite and schist of Panjerli Formation; quartzite unit of Manal Formation; phyllite, schist and quartzite of Bhotli Formation; quartzite unit of Khirki Formation and carbonaceous schist, crystalline limestone of Taradevi Formation.
S0 and S1 are the prominent planar surfaces with local development of S2 and S3. F1, F2 and F3 are the three generations of folds. F1 is in minor scale as appressed and reclined folds related to tectonic transport and F2 and F3 having formed after the emplacement of the thrust sheet. F2 is the most pervasive structure along NW-SE, folding the klippe into an open synform. F3 is a larger cross-fold along WSW-ENE and is responsible for culminations and depressions of F2 folds.
The direction of tectonic transport is from ENE to WSW and F2 folds indicate a compression along the same direction.
- Contemporary Geoscientific Researches in Himalaya
Abstract Views :203 |
PDF Views:120
Authors
Affiliations
1 Geological Survey of India, Bangalore, IN
1 Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 4 (1985), Pagination: 295-297Abstract
No Abstract.Full Text
- Tertiary Fishes and Molluscs from the Kuksho Formation of the Indus Group, Near Nyoma, Ladakh
Abstract Views :182 |
PDF Views:4
Authors
Affiliations
1 Department of Geology, Punjab University, Chandigarh, IN
2 Department of Geology, 2, Church Street, Bangalore-560 001, IN
3 Department of Geology, Madras, IN
4 Department of Geology, Srinagar, IN
1 Department of Geology, Punjab University, Chandigarh, IN
2 Department of Geology, 2, Church Street, Bangalore-560 001, IN
3 Department of Geology, Madras, IN
4 Department of Geology, Srinagar, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 25, No 11 (1984), Pagination: 744-747Abstract
A collection of Tertiary fishes and molluscs from the Kuksho Formation of the Indus Group near Nyoma, Ladakh are described, The fish families represented are: Siluridae, Channidae and Cyprinidae. The fishes are associated with dextrally coiled gastropods and unionid pelecypods.- 'Chail Series' of the Himachal Himalaya
Abstract Views :444 |
PDF Views:4
Authors
Affiliations
1 1116, 10th Cross, Banasankari 1st Stage, II Block, Bangalore 560050, IN
2 529, Sector 18-C, Chandigarh 160018, IN
1 1116, 10th Cross, Banasankari 1st Stage, II Block, Bangalore 560050, IN
2 529, Sector 18-C, Chandigarh 160018, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 5 (1985), Pagination: 350-355Abstract
A critical study brings out that the 'Chail Series' broadly occurs in two tectonic positions - the 'Lower Chail allochthon' as a thrust sheet over the Shali and the' Upper Chail allochthon' as an infra-Jutogh thrust sheet. The revision mapping of the Simla area has brought out that the' Lower Chail allochthon' includes (i) a sedimentary unit occurring as a cover over the Shali and designated as the Basantpur Formation of the Simla Group and (ii) a regional nappe tectonically overlying the Shali-Simla Groups and designated as the Salkhala thrust sheet. The' Upper Chail allochthon' has been found to be part of the Jaunsar Group. Thus, the' Chail ' was never an entity and has lost its validity as a stratigraphic term. This naturally precludes its adoption even as a tectonic term.- Kuppalapalle Volcanics - A Distinct Upper Papaghni Volcanic Activity in the Cuddapah Basin
Abstract Views :162 |
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Authors
Affiliations
1 1116, 10th Cross, Banasankari First Stage, II Block, Bangalore 560 050, IN
1 1116, 10th Cross, Banasankari First Stage, II Block, Bangalore 560 050, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 25, No 12 (1984), Pagination: 775-779Abstract
The volcanic episode in the Cuddapah Basin requires to be given a specific position in the stratigraphic column, as volcanics occupy definite position in time and space. Kuppalapalle Volcanics is the new name proposed for a distinct Upper Papaghni phase of volcanic activity which is post-Vempalle and pre-Pulivendla, representing a sequence of several lava flows.- Himalayan Shears
Abstract Views :194 |
PDF Views:117
Authors
Affiliations
1 A.M.S.E. Wing, G.S.I., Bangalore, IN
1 A.M.S.E. Wing, G.S.I., Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 25, No 12 (1984), Pagination: 812-813Abstract
No Abstract.Full Text
- Archaean Komatiites from Banasandra Area of Kibbanahalli Arm Of Chitradurga Supracrustal Belt in Karnataka
Abstract Views :260 |
PDF Views:2
Authors
Affiliations
1 Geological Survey of India, No.2, Church Street, Bangalore 560001, IN
1 Geological Survey of India, No.2, Church Street, Bangalore 560001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 6 (1985), Pagination: 407-417Abstract
The Banasandra Komatiites occur within the Kibbanahalli arm of the Chitradurga supracrustal Belt in Karnataka. They apparently overlie the Bababudan Group and the Peninsular Gneiss and occur in two isolated exposures, (i) east of Birasandra, and (ii) near Kodihalli - Kunikenahalli. Ultramafic rock types include pillowed serpentinites, spinifex-textured komatiite, massive and schistose serpentinite and talc-tremolite-chlorite schist. Certain quartz-antigorite (birbirite ?), quartz-amphibole, and high-magnesian chlorite rocks are also closely associated with the ultramafics. The major element chemistry of the Banasandra komatiites compares with those of Barberton, S. Africa, Munro Township, Canada and of W. Australia. The exact relationship between these komatiites and the Bababudan volcanics is not clear for lack of continuous outcrops. Field evidences point to possible tectonic emplacement.- Trilobite and Other Trace Fossils from the Kunzam La Formation, Eastern Lahaul Valley, Himachal Himalaya
Abstract Views :202 |
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Authors
Affiliations
1 529, Sector 18B, Chandigarh 160 018, IN
2 1116, 10th Cross, BSK, 1st Stage, Bangalore 560 050, IN
1 529, Sector 18B, Chandigarh 160 018, IN
2 1116, 10th Cross, BSK, 1st Stage, Bangalore 560 050, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 12 (1985), Pagination: 880-886Abstract
Trilobite locomotion trail Isopodichnus sp., swimming grazing trace Monomorphichnus sp. and resting trace Rusophycus didymus are recorded from the siltstone-shale-quartzarenite sequence of the Kunzam La Formation (Cambrian) from the eastern Lahaul Valley, Himachal Himalaya. Besides these, a ringed conical ichnocoenosis is also reported.
The trilobite traces belong to Cruziana 'facies' which is characteristic of stable infra-littoral to circa-littoral zones. The presence of Rusophycus suggests a rather low energy environment.
- Aspects of Tectonics - Focus on South-Central Asia
Abstract Views :181 |
PDF Views:111
Authors
Affiliations
1 A.M.S.E. Wing, Geological Survey of India, Bangalore 560 001, IN
1 A.M.S.E. Wing, Geological Survey of India, Bangalore 560 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 12 (1985), Pagination: 899-901Abstract
No Abstract.Full Text
- Proceedings of the Krol - Tal, Field Meeting 25-27
Abstract Views :203 |
PDF Views:118
Authors
Affiliations
1 A.M.S.E. Wing, Geological Survey of India, Bangalore, IN
1 A.M.S.E. Wing, Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 27, No 4 (1986), Pagination: 401-401Abstract
No Abstract.Full Text
- Geology of the Bhutan Himalaya
Abstract Views :172 |
PDF Views:122
Authors
Affiliations
1 A.M.S.E. Wing, Geological Survey of India, Bangalore., IN
1 A.M.S.E. Wing, Geological Survey of India, Bangalore., IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 27, No 2 (1986), Pagination: 236-239Abstract
No Abstract.Full Text
- Himalayan Thrusts and Structural Belts
Abstract Views :175 |
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Authors
Affiliations
1 Geological Survey of India, IN
1 Geological Survey of India, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 31, No 2 (1988), Pagination: 210-229Abstract
The Himalayan Orogen is characterised by a series of linear and parallel thrusts demarcating individual tectono-stratigraphic units. Two major tectogens, the Lesser Himalayan and the Tethyan, are recognised and these are separated by the Main Central Thrust (MCT). The MCT is the most fundamental of all thrusts in the Himalaya and represents the outermost tectonic transgression of the crystalline thrust nappes with or without Phanerozoic Tethyan cover over the Lesser Himalayan tectogen. The MCT can be recognised all along the Himalaya and is invariably characterised by retrogressive metamorphic characters and schuppen structures. It also comprises sub-nappes like the Salkhala and the Jutogh in the NW Himalaya.The Lesser Himalayan Tectogen has several structural belts demarcated by well-defined thrust planes and imbricate zones. The Himachal Himalaya has the maximum development of these structural belts.
Another important aspect of Lesser Himalayan tectogen is the extensive detachment of cover rocks along the planes of unconformity or even bedding.
Along the northern margin of the Tethys Himalayan tectogen, the thrust sheets generally have a NE-directed movement, whereas along the southern margin the thrust sheets have SW-directed movement. The highest allochthon in the Himalaya is represented by the Shilakong and Jungbwa ophiolite nappes.
The Indus Tectonic Zone borders the Himalaya along its northern margin and is represented by two structural belts viz. the Sangeluma and Indus belts.
- Contribution to the History of Geological Mapping
Abstract Views :183 |
PDF Views:114
Authors
Affiliations
1 A. M. S. E. Wing, Geological Survey of India, Bangalore 560 001, IN
1 A. M. S. E. Wing, Geological Survey of India, Bangalore 560 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 30, No 4 (1987), Pagination: 320-322Abstract
No Abstract.Full Text
- Sheet Evolution of Continents a Morpho-Structural Approach
Abstract Views :185 |
PDF Views:115
Authors
Affiliations
1 A. M. S. E. Wing, Geological Survey of India, Bangalore, IN
1 A. M. S. E. Wing, Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 31, No 3 (1988), Pagination: 353-353Abstract
No Abstract.Full Text
- Scientific Report of Third Indian Expedition to Antarctica
Abstract Views :185 |
PDF Views:103
Authors
Affiliations
1 A.M.S.E. Wing, Geological Survey of India, Bangalore, IN
1 A.M.S.E. Wing, Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 30, No 6 (1987), Pagination: 540-541Abstract
No Abstract.Full Text
- Ophiolite and Indian Plate Margin
Abstract Views :182 |
PDF Views:97
Authors
Affiliations
1 A.M.S.E. Wing, Geological Survey of India, Bangalore, IN
1 A.M.S.E. Wing, Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 32, No 2 (1988), Pagination: 148-149Abstract
No Abstract.Full Text
- Aspects of Fluvial Sedimentation in the Lower Triassic Buntsandstein of Europe
Abstract Views :220 |
PDF Views:128
Authors
Affiliations
1 Geological Survey of India, AMSE Wing, Bangalore, IN
1 Geological Survey of India, AMSE Wing, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 32, No 3 (1988), Pagination: 254-255Abstract
No Abstract.Full Text
- The Jutogh Group of Metasediments of the Himachal Himalaya: Its Lithostratigraphy
Abstract Views :214 |
PDF Views:2
Authors
Affiliations
1 1116, 10th Cross, Banasankari L Stage, II Block, Bangalore 560050, IN
2 529, Sector 18-B, Chandigarh 160 018, IN
1 1116, 10th Cross, Banasankari L Stage, II Block, Bangalore 560050, IN
2 529, Sector 18-B, Chandigarh 160 018, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 32, No 4 (1988), Pagination: 279-294Abstract
The Jutogh Group of the Himachal Himalaya is divisible into eleven formations based on normal order of superposition, lithological association, lateral persistence and systematic mapping. This study helps greatly in reconstructing the sedimentary history, structural evolution and promoting better inter-regional correlation.- The Archaean Komatiites of Nagamangala Supracrustal Belt, Karnataka
Abstract Views :207 |
PDF Views:2
Authors
Affiliations
1 A. M. S. E. Wing, Geological Survey of India, No.2, Church Street, Bangalore 560001, IN
1 A. M. S. E. Wing, Geological Survey of India, No.2, Church Street, Bangalore 560001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 33, No 3 (1989), Pagination: 210-214Abstract
The meta-ultramafites of the Archaean Nagamangala belt of Karnataka craton display pillow structures and have kornatiitic chemistry. This is in conformity with other ancient supracrustals of Karnataka craton having komatiitic association.- Tectonics of the Western Himalayas
Abstract Views :187 |
PDF Views:126
Authors
Affiliations
1 Geological Survey of India, Bangalore, IN
1 Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 37, No 1 (1991), Pagination: 91-92Abstract
No Abstract.Full Text
- Unusual Concentric Structures in Komatiite of Kibbanahalli Arm of Chitradurga Supracrustal Belt near Banasandra, Karnataka
Abstract Views :179 |
PDF Views:2
Authors
S. V. Srikantia
1,
M. S. Rao
1
Affiliations
1 A. M. S. E. Wing, Geological Survey of India, No.2, Church Street, Bangalore 560001, IN
1 A. M. S. E. Wing, Geological Survey of India, No.2, Church Street, Bangalore 560001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 36, No 4 (1990), Pagination: 424-429Abstract
The occurrence of unusual concentric structures in a serpentinite band of the Banasandra Komatiite Complex of the Kibbanahalli arm, Chitradurga Supracrustal belt is recorded. These structures, along with spinifex textured and pillowed serpentinite appear to be flow-related.Keywords
Petrography, Komatiites, Kibbanahalli, Chitradurga Belt, Banasandra, Karnataka.- Proceedings of the National Seminar of Tertiary Orogeny in Indian Subcontinent, 1987
Abstract Views :173 |
PDF Views:128
Authors
Affiliations
1 Geological Survey of India Bangalore, IN
1 Geological Survey of India Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 37, No 3 (1991), Pagination: 307-308Abstract
No Abstract.Full Text
- Annual Report 1988-89, Wadia Institute of Himalayan Geology
Abstract Views :204 |
PDF Views:107
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 37, No 4 (1991), Pagination: 412-413Abstract
No Abstract.Full Text
- Discussion
Abstract Views :205 |
PDF Views:116
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 38, No 6 (1991), Pagination: 632-633Abstract
No Abstract.Full Text
- Glacial and Fluvial Geomorphology of Western Himalaya
Abstract Views :185 |
PDF Views:114
Authors
Affiliations
1 Geological Survey of India, Bangalore, IN
1 Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 39, No 4 (1992), Pagination: 355-355Abstract
No Abstract.Full Text
- Workshop on Vindhyan Stratigraphy and Palaeobiology, March 19-20,1999, Lucknow
Abstract Views :194 |
PDF Views:158
Authors
Affiliations
1 Geological Society of India, Bangalore, IN
1 Geological Society of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 53, No 6 (1999), Pagination: 724-726Abstract
No Abstract.Full Text
- Geology of the Lower Himalaya (Garhwal)
Abstract Views :172 |
PDF Views:106
Authors
Affiliations
1 Flat-201, A Block, Ushas Apts., 26, 16th Main, IV Block, Jayanagar, Bangalore-560011, IN
1 Flat-201, A Block, Ushas Apts., 26, 16th Main, IV Block, Jayanagar, Bangalore-560011, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 44, No 2 (1994), Pagination: 224-225Abstract
No Abstract.Full Text
- Non-Availability of Geological Maps - The Bane of Indian Geology
Abstract Views :164 |
PDF Views:1
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 46, No 1 (1995), Pagination: 1-4Abstract
No Abstract.- Geonews
Abstract Views :174 |
PDF Views:105
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 46, No 5 (1995), Pagination: 575-576Abstract
No Abstract.Full Text
- Geology of Western Himalaya 1993
Abstract Views :179 |
PDF Views:176
Authors
Affiliations
1 201A, Ushas Apts., 26, 16th Main, Jayanagar 4th Block, Bangalore - 560 011, IN
1 201A, Ushas Apts., 26, 16th Main, Jayanagar 4th Block, Bangalore - 560 011, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 45, No 4 (1995), Pagination: 487-489Abstract
No Abstract.Full Text
- Geological Society of India Library
Abstract Views :160 |
PDF Views:97
Authors
Affiliations
1 Geological Society of India Bangalore - 560 019, IN
1 Geological Society of India Bangalore - 560 019, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 45, No 4 (1995), Pagination: 491-491Abstract
No Abstract.Full Text
- Geo Karnataka - Mysore Geological Department Centenary Volume 1994
Abstract Views :146 |
PDF Views:116
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 46, No 4 (1995), Pagination: 452-453Abstract
No Abstract.Full Text
- Geology and Mineral Resources of Orissa
Abstract Views :170 |
PDF Views:116
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 46, No 2 (1995), Pagination: 201-201Abstract
No Abstract.Full Text
- Himalayan Orogen and Global Tectonics
Abstract Views :177 |
PDF Views:109
Authors
Affiliations
1 Geological Survey of India, Bangalore, IN
1 Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 42, No 2 (1993), Pagination: 207-207Abstract
No Abstract.Full Text
- The Rhomboid Protractor and its Application in the Construction of Isometric Geological Panel Diagrams
Abstract Views :198 |
PDF Views:110
Authors
Affiliations
1 Chandigarh, IN
1 Chandigarh, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 14, No 1 (1973), Pagination: 101-104Abstract
No Abstract.Full Text
- Orbicular Rocks from Closepet Granite Near Hoskote, Tumkur Dt., Karnataka
Abstract Views :189 |
PDF Views:1
Authors
Affiliations
1 Geological Survey of India, Bangalore-560 011, IN
1 Geological Survey of India, Bangalore-560 011, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 43, No 3 (1994), Pagination: 267-279Abstract
The paper records the first occurrence of Orbicular rocks from the Closepet Granitoid belt near Hoskote, Tumkur district, Karnataka. The orbicules occur in a dioritic country rock enclosed within grey Closepet Granitoid. These are multishelled orbicules with shells of plagioclase and hornblende with a core of the same minerals. There are also proto-orbicules. The chemical analyses of orbicules fall in mafic tonalite field on K2O - CaO plots. Individual shells reflect a basic rock parentage. The orbicules are derived from a metabasic enclave due to granitic action by melting, diffusion and concretionary process in hydrous stage.Keywords
Closepet Granites, Orbicules, Igneous Petrology, Hoskote, Tumkur, Karnataka.- Symposium on Recent Advances in Geological Studies of the Northwest Himalaya and the Foredeep
Abstract Views :182 |
PDF Views:95
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 48, No 3 (1996), Pagination: 365-367Abstract
No Abstract.Full Text
- Professor S.S. Merh Honoured
Abstract Views :174 |
PDF Views:120
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 48, No 6 (1996), Pagination: 710-710Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting for 1995-96
Abstract Views :185 |
PDF Views:113
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 48, No 6 (1996), Pagination: 711-712Abstract
No Abstract.Full Text
- International Symposium on Granulite Facies Rocks
Abstract Views :194 |
PDF Views:111
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 3 (1997), Pagination: 337-338Abstract
No Abstract.Full Text
- The Talkad Sand Dunes in Mysore District of Karnataka - their Description, Evolution and Origin
Abstract Views :234 |
PDF Views:2
Authors
Affiliations
1 A-201, Ushas Apts. 26, 16th Main, Jayanagar IV Block, Bangalore - 560 011, IN
2 Geological Survey of India, Kumaraswamy Layout, Bangalore - 560 078, IN
1 A-201, Ushas Apts. 26, 16th Main, Jayanagar IV Block, Bangalore - 560 011, IN
2 Geological Survey of India, Kumaraswamy Layout, Bangalore - 560 078, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 50, No 3 (1997), Pagination: 315-321Abstract
Situated along the left bank of the river Cauvery, Talakad represents a typical riverine sand dune. The point bar deposit along the left bank of the Cauvery is the main source of the sand. However, this stretch, in the upstream has a weir built some 400 years ago which diverted water from the Cauvery into the Madha vamantri canal, which resulted in the lowering of the level of water in the point bar deposit downstream thereby exposing its sand to monsoonic winds blowing from SW to NE towards Old Talkad. The settlements and also the NW to SE blowing cross wind in the valley acted as barriers for the sand laden monsoonic winds with the consequent development of sand dunes which on gradual migration buried temples and many old settlements.Keywords
Geomorphology, Sand Dunes, River Cauvery, Karnataka.- Gis and Geological Remote Sensing
Abstract Views :180 |
PDF Views:103
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 50, No 1 (1997), Pagination: 113-114Abstract
No Abstract.Full Text
- Dimensions of Himalayan Geology
Abstract Views :214 |
PDF Views:109
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 72, No 4 (2008), Pagination: 573-574Abstract
No Abstract.Full Text
- A. R. Gokul (1924-2008)
Abstract Views :179 |
PDF Views:114
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 71, No 4 (2008), Pagination: 602-602Abstract
No Abstract.Full Text
- Mohammed Ziauddin (1923-2008)
Abstract Views :201 |
PDF Views:120
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 71, No 5 (2008), Pagination: 751-751Abstract
No Abstract.Full Text
- The Stratigraphy, Sedimentology and Basin Evolution of the Natal Group
Abstract Views :181 |
PDF Views:108
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 67, No 6 (2006), Pagination: 809-810Abstract
No abstract.Full Text
- Proceedings of the Workshop on Gangotri Glacier
Abstract Views :161 |
PDF Views:149
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 68, No 2 (2006), Pagination: 328-330Abstract
No Abstract.Full Text
- J. S. Venugopal (1935-2006)
Abstract Views :150 |
PDF Views:114
Authors
Affiliations
1 Geological Society of India, Bangalore - 560 019, IN
1 Geological Society of India, Bangalore - 560 019, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 68, No 4 (2006), Pagination: 737-738Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting - 2003-2004 at Visakhapatnam
Abstract Views :169 |
PDF Views:123
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 65, No 1 (2005), Pagination: 107-111Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting-2002-2003 at Vasco Da Gama, Goa
Abstract Views :181 |
PDF Views:119
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 63, No 1 (2004), Pagination: 103-106Abstract
No Abstract.Full Text
- Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic Process
Abstract Views :193 |
PDF Views:139
Authors
Affiliations
1 Geological Society of India, Bangalore - 560 01 9, IN
1 Geological Society of India, Bangalore - 560 01 9, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 63, No 6 (2004), Pagination: 682-684Abstract
No Abstract.Full Text
- J. Swami Nath (1924-2003)
Abstract Views :166 |
PDF Views:120
Authors
Affiliations
1 Geological Society of India, Bangalore, IN
1 Geological Society of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 62, No 3 (2003), Pagination: 386-387Abstract
No Abstract.Full Text
- Notice of Monthly Meetings
Abstract Views :165 |
PDF Views:111
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 59, No 1 (2002), Pagination: 3-3Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting for 1999-2000
Abstract Views :183 |
PDF Views:110
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 57, No 1 (2001), Pagination: 85-87Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting for 2000-2001
Abstract Views :171 |
PDF Views:109
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 58, No 6 (2001), Pagination: 545-547Abstract
No Abstract.Full Text
- Who should Head the Geological Survey of India
Abstract Views :179 |
PDF Views:110
Authors
Affiliations
1 Geological Society of India, Bangalore, IN
1 Geological Society of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 58, No 3 (2001), Pagination: 273-273Abstract
No Abstract.Full Text
- Geological Map of India
Abstract Views :185 |
PDF Views:180
Authors
Affiliations
1 Geological Society of India, Bangalore, IN
1 Geological Society of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 58, No 3 (2001), Pagination: 276-277Abstract
No Abstract.Full Text
- Proceedings of the Annual General Meeting - 2001-2002
Abstract Views :170 |
PDF Views:104
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 61, No 1 (2003), Pagination: 103-105Abstract
No Abstract.Full Text
- Lakes: Water and Sediment Geochemistry
Abstract Views :194 |
PDF Views:127
Authors
Affiliations
1 Geological Society of India, IN
1 Geological Society of India, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 74, No 2 (2009), Pagination: 275-276Abstract
No Abstract.Full Text
- Dynamic Himalaya
Abstract Views :183 |
PDF Views:133
Authors
Affiliations
1 Geological Society of India, Bangalore - 560 019, IN
1 Geological Society of India, Bangalore - 560 019, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 52, No 6 (1998), Pagination: 743-744Abstract
No Abstract.Full Text
- Fifty Years of Indian Earth Science After Independence
Abstract Views :206 |
PDF Views:2
Authors
Affiliations
1 Geological Society of India, IN
1 Geological Society of India, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 50, No 2 (1997), Pagination: 125-130Abstract
No Abstract.- International Seminar on Quaternary Sea-Level Variation, Shoreline Displacement and Coastal Environment, Thanjavur (20-26 Jan. 1997)
Abstract Views :181 |
PDF Views:120
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 50, No 2 (1997), Pagination: 236-237Abstract
No Abstract.Full Text
- Exploration and Exploitation of Gold Resources of India
Abstract Views :176 |
PDF Views:122
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 5 (1997), Pagination: 601-602Abstract
No Abstract.Full Text
- Himalayan Thrusts and Associated Rocks
Abstract Views :170 |
PDF Views:110
Authors
Affiliations
1 A. M. S. E. Wiug, Geological Survey of India, Bangalore, IN
1 A. M. S. E. Wiug, Geological Survey of India, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 29, No 2 (1987), Pagination: 279-280Abstract
No Abstract.Full Text
- Geology in School Education
Abstract Views :165 |
PDF Views:1
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 47, No 6 (1996), Pagination: 645-648Abstract
No Abstract.- Foundation Day of Geological Society of India: Group discussion on Mining and Environment
Abstract Views :730 |
PDF Views:218
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 80, No 3 (2012), Pagination: 440-445Abstract
No Abstract.Full Text
- Augusto Gansser (1910 – 2012)
Abstract Views :206 |
PDF Views:0
Authors
Affiliations
1 Bangalore, IN
1 Bangalore, IN