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Co-Authors
- Gauri Dole
- V. V. Peshwa
- Sushma Nair
- Shilpa Patil
- V. G. Phansalkar
- Anand S. Kale
- Nitin R. Karmalkar
- Vaishali Ghunakikar
- P. Paul Thomas
- Ashok Kaushal
- Shilpa Patil Pillai
- Mukund Sharma
- Manoj Shukla
- Shilpa S. Patil
- Vidyadhar Satoskar
- Prakhar Kumar
- S. Viswanathan
- K. S. Misra
- Ninad Bondre
- Raymond A. Duraiswami
A B C D E F G H I J K L M N O P Q R S T U V W X Y Z All
Kale, Vivek S.
- Evidence of a Palaeoseismic Event from the Deccan Plateau Uplands
Abstract Views :156 |
PDF Views:2
Authors
Affiliations
1 Department of Geology, University of Pune, Pune 411007, IN
1 Department of Geology, University of Pune, Pune 411007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 56, No 5 (2000), Pagination: 547-555Abstract
Palaeoseismic evidence is recorded for the first time from the upland region near the crest of the Deccan plateau. Some of the soft-sediment deformation structures from Quaternary sediments in the Chandanapuri valley are interpreted as seismites. These sediments rest nonconformably upon the Deccan Traps and are inherently anomalous vis-a-vis their location in the river valley. Based on various features and their position in the succession of the sediments, these seismites are provisionally attributed to a single event with an inferred magnitude > 6.5 M, which occurred 5000 - 7000 years ago. This report highlights the need to re-evaluate the traditional perception of the aseismic nature of the main Deccan plateau.Keywords
Palaeoseismology, Deccan Plateau, Quaternary Sediments, Seismites.
- Testimony of Intraformational Limestone Breccias on Lokapur-Simikeri Disconformity, Kaladgi Basin
Abstract Views :180 |
PDF Views:3
Authors
Affiliations
1 Department of Geology, University of Pune, Pune-411 007, IN
1 Department of Geology, University of Pune, Pune-411 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 51, No 1 (1998), Pagination: 43-48Abstract
Detailed measurements of a more than 55 m wide tract of the Chikshellikeri Limestone, immediately underlying the Muchkundi Quartzite were undertaken in the Kaladgi Basin. This sequence is constituted of 3218 measured laminations from more than 1550 mudstone - packstone couplet. They are interrupted by 57 horizons of Intraformational Limestone Breccias. The distribution pattern of these horizons within the sequence is evaluated within the framework of the depositional environments which yielded the limestone sequence and they are recognised as products of events of penecontemporaneous basin-floor instability. It is shown that disconformity separating the Bagalkot Group into two Subgroups (earlier attributed to two separate transgresive events) was formed as a result of reorganisation of the basin configuration in response to synsedimentary tectonics and not as a result of a second transgression of the contemporary sea.Keywords
Sedimentology, Kaladgi Basin, Disconformity, Meso- Neoproterozoic, Basin Evolution, Karnataka.- Carbonates Intertropicaux [Intertropical Carbonates]
Abstract Views :159 |
PDF Views:125
Authors
Affiliations
1 Department of Geology, University of Pune, Pune-411 007, IN
1 Department of Geology, University of Pune, Pune-411 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 51, No 1 (1998), Pagination: 127-128Abstract
No Abstract.Full Text
- Occurrence and Significance of Algal Stromatolites from the Choral Valley, Near Barwah, Khargoan District, M.P.
Abstract Views :187 |
PDF Views:2
Authors
Affiliations
1 Department of Geology, University of Poona, Pune 411 007, IN
1 Department of Geology, University of Poona, Pune 411 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 10 (1985), Pagination: 751-756Abstract
Conophytoll cylindricus, Collenia columnaris, Collenia symmetrica and Collenia undosa are reported from the dolomitic intercalations within the Mehdikhera Chertbreccia Formation, exposed in the Choral river valley near Barwah, in Khargoan District, Madhya Pradesh. There is a lack of consensus regarding the origin of this Formation and it has been considered to be equivalent of Bijawars. The present report of stromatolites conclusively points to its sedimentary origin and suggests a need for a reappraisal of the age.- An Unusual Evaporite Association from the Papaghni Group, Cuddapah Basin
Abstract Views :183 |
PDF Views:1
Authors
Affiliations
1 Department of Geology, University of Poona, Pune 411007, IN
1 Department of Geology, University of Poona, Pune 411007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 37, No 1 (1991), Pagination: 75-79Abstract
The hitherto unreported occurrence of halite and gypsum casts from the Vempalle Formation is reported. Implications in terms of the early depositional history of the Cuddapah Basin is discussed.Keywords
Vempalle Formation, Cuddapah Basin, Papaghni Group, Evaporite, Andhra Pradesh.- The Vendian System (Vol. 2: Regional Geology)
Abstract Views :248 |
PDF Views:128
Authors
Affiliations
1 Department of Geology, University of Poona, IN
1 Department of Geology, University of Poona, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 37, No 5 (1991), Pagination: 506-507Abstract
No Abstract.Full Text
- Constraints on the Evolution of the Purana Basins of Peninsular India
Abstract Views :193 |
PDF Views:1
Authors
Affiliations
1 Department of Geology, University of Poona, Pune 411 007, IN
1 Department of Geology, University of Poona, Pune 411 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 38, No 3 (1991), Pagination: 231-252Abstract
The seven supracrustal, epicratonic Purana basins occupy more than a fifth of the area of Precambrian exposures in the Indian Shield. They are repositories of Proterozoic shallow marine sediments, resting unconformably on the eroded surfaces of the older rocks; and are preserved in an unmetamorphosed and marginally deformed state. These sequences have comparable characters though their mutual differences are quite significant, indicating that each one of the host basins had an independent evolutionary history.
The gross sedimentological contents, associated igneous rocks, structural and metamorphic features of the Purana basins and their geographical and temporal proximity with the Middle Proterozoic Mobile Belt are examined to evaluate the broad geotectonic framework within which they evolved. These "polyhistory, continental" basins are apparently analogous to the "Atlantic-type" passive continental margin systems associated with extensional tectonic regimes. The Bhima basin is an exceptional case of a "simple", transtensional, "pull-apart" type basin, while some of the others were probably initiated as "back-arc" basins.
- IGCP 264: Remote Sensing Spectral Properties Report of the Pune (India) Meeting-1991
Abstract Views :210 |
PDF Views:154
Authors
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 39, No 3 (1992), Pagination: 262-263Abstract
No Abstract.Full Text
- Annual General Meeting 1995 : A Report
Abstract Views :200 |
PDF Views:119
Authors
Affiliations
1 Department of Geology, University of Pona, Pune-411007, IN
1 Department of Geology, University of Pona, Pune-411007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 46, No 6 (1995), Pagination: 680-682Abstract
No Abstract.Full Text
- Macrofacies Architecture of the First Transgressive Suite Along the Southern Margin of the Kaladgi Basin
Abstract Views :232 |
PDF Views:1
Authors
Affiliations
1 Department of Geology, University of Pune, Pune-411 007, IN
1 Department of Geology, University of Pune, Pune-411 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 48, No 1 (1996), Pagination: 75-92Abstract
The lowest sequence of the Lokapur Subgroup from the Bagalkot Group manifests the earliest transgression in the Meso-Neoproterozoic Kaladgi Basin. It is characterised by four sedimentary lithofacies namely, (i) sandstone facies (dominantly quartzose-arenites with minor interbedded conglomerates and gravel beds), (ii) argillite facies (including siltstones and shales), (iii) carbonate facies (primarily dolomites which are often cherty and stromatolitic) and, (iv) chertbreccia facies (poorly bedded and silicified).
These four macrofacies have been studied in the gently folded and faulted exposures along the southern margin of the Kaladgi Basin. An unfolded fence of their distribution and mutual dispositions is reconstructed so as to enable the visualization of their syndepositional architecture. Modifications of the existing classification of the examined sequence of the Lokapur Subgroup are suggested on the basis of this restoration and in context of process responsive lithostratigraphy.
The Kaladgi Basin is interpreted to have been initiated in an extensional tectonic regime. All the four recognised macrofacies were deposited more or less simultaneously during the earliest transgression in this basin and their architecture was governed by synsedimentary events of sagging of the uneven basin floor along an array of East-West trending growth faults with northern downthrows.
Keywords
Sedimentology, Meso-Neoproterozoic, Kaladgi Basin, Karnataka.- Remote Sensing for Natural Resources With Special Emphasis on Water Management
Abstract Views :201 |
PDF Views:116
Authors
Affiliations
1 Geology Department,Pune University, Pune, IN
1 Geology Department,Pune University, Pune, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 3 (1997), Pagination: 339-340Abstract
No Abstract.Full Text
- Purana Basins of Karnataka
Abstract Views :172 |
PDF Views:122
Authors
Affiliations
1 Kalyani Net Ventures Ltd, lndustry House, S No 48, Mundhwa, Pune-411036, IN
1 Kalyani Net Ventures Ltd, lndustry House, S No 48, Mundhwa, Pune-411036, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 71, No 2 (2008), Pagination: 293-294Abstract
No Abstract.Full Text
- Online Databases and other Internet Resources for Earth Sciences
Abstract Views :172 |
PDF Views:118
Authors
Affiliations
1 Kalyani Net Ventures Ltd., Pune 411 036, IN
1 Kalyani Net Ventures Ltd., Pune 411 036, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 71, No 3 (2008), Pagination: 433-434Abstract
No Abstract.Full Text
- Coastal Environments: Problems and Perspectives
Abstract Views :203 |
PDF Views:121
Authors
Affiliations
1 Pune, IN
1 Pune, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 74, No 5 (2009), Pagination: 651-651Abstract
No Abstract.Full Text
- Anant V. Phadke (1937-2010)
Abstract Views :223 |
PDF Views:101
Authors
Affiliations
1 Pune, IN
1 Pune, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 76, No 3 (2010), Pagination: 294-294Abstract
No Abstract.Full Text
- Occurrence of a Manganese-Bearing Horizon in the Kaladgi Basin
Abstract Views :159 |
PDF Views:2
Authors
Shilpa Patil Pillai
1,
V. V. Peshwa
1,
Sushma Nair
1,
Mukund Sharma
2,
Manoj Shukla
2,
Vivek S. Kale
1
Affiliations
1 Department of Geology, University of Pune, Pune 411007, IN
2 Birbal Sahni Institute of Palaeobotany, Lucknow 226007, IN
1 Department of Geology, University of Pune, Pune 411007, IN
2 Birbal Sahni Institute of Palaeobotany, Lucknow 226007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 53, No 2 (1999), Pagination: 201-204Abstract
A manganiferous horizon was recorded near Niralkeri, in an intricately folded quartzite-chert breccia-mudstone sequence of the Simikeri Subgroup in the Kaladgi Basin of Karnataka. The nodules collected from this horizon show the presence of todorokite, vemadite and lithophorite in association with quartz and hematite; with MnO-58%.Keywords
Economic Geology, Manganese, Proterozoic, Kaladgi Basin, Karnataka.- Occurrence of Planolites from the Nagarjuna Sagar Area, Northwestern Cuddapah Basin
Abstract Views :168 |
PDF Views:127
Authors
Affiliations
1 Department of Geology, University of Pune, Pune - 411 007, IN
2 Atomic Minerals Division, D.A.E., Hyderabad - 500016, IN
1 Department of Geology, University of Pune, Pune - 411 007, IN
2 Atomic Minerals Division, D.A.E., Hyderabad - 500016, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 5 (1997), Pagination: 589-596Abstract
This note records the presence and systematics of ichnogenus Planolites Nicholson from the Cuddapah Basin. The host sandstones are exposed in the Nalgonda district of Andhra Pradesh, on the border between Palnad and Srisailam subbasins of the Cuddapah Basin. Planolites is known to occur in strata of Neoproterozoic and younger ages.Full Text
- Arterial System of Lava Tubes and Channels within Deccan Volcanics of Western India
Abstract Views :171 |
PDF Views:162
Authors
S. Viswanathan
1,
K. S. Misra
2,
Gauri Dole
3,
Ninad Bondre
4,
Raymond A. Duraiswami
5,
Vivek S. Kale
6
Affiliations
1 10, Bapuji Apts., Rajendra Prasad Raod, Dombivli (East) - 421 201, IN
2 Geological Survey of India, Alandi Road, Phule Nagar, Pune - 411 006, IN
3 238, Narayan Felli, Pune, 411 030, IN
4 114 Shideler Hall, Department of Geology, Miami University, Oxford, Ohio 45056, US
5 A16 Gurudut Housing Society, Srinagar, Kalewadi Phatta, Rahatani, Pune - 411 017, IN
6 Kalyani Net Ventures Ltd., Pune, IN
1 10, Bapuji Apts., Rajendra Prasad Raod, Dombivli (East) - 421 201, IN
2 Geological Survey of India, Alandi Road, Phule Nagar, Pune - 411 006, IN
3 238, Narayan Felli, Pune, 411 030, IN
4 114 Shideler Hall, Department of Geology, Miami University, Oxford, Ohio 45056, US
5 A16 Gurudut Housing Society, Srinagar, Kalewadi Phatta, Rahatani, Pune - 411 017, IN
6 Kalyani Net Ventures Ltd., Pune, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 60, No 5 (2002), Pagination: 595-600Abstract
No Abstract.Full Text
- A Reinterpretation of Two Chertbreccias from the Proterozoic Basins of India
Abstract Views :247 |
PDF Views:1
Authors
Affiliations
1 Kalyani Global Engineering Pvt. Ltd., Industry House, Mundhwa, Pune - 411 036, IN
2 Sinhgad College of Science, Pune - 411 0041, IN
1 Kalyani Global Engineering Pvt. Ltd., Industry House, Mundhwa, Pune - 411 036, IN
2 Sinhgad College of Science, Pune - 411 0041, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 78, No 5 (2011), Pagination: 429-445Abstract
Several horizons of a unique lithotype called "chertbreccia" are interbedded within the Proterozoic platform sediments of the Peninsular India. These cherty rocks with brecciated texture appearing as blocky masses were earlier diversely interpreted as being products of disparate processes such as fault-zone breccias, collapse breccias, and so on. Two of these horizons, one from the Kaladgi Basin (Dharwar Craton) and the other from the Dhar Forest Inlier of the Vindhyanchal Basin (Bundelkhand - Aravalli Craton) are compared in context of their geological setting, field relations and petrological constitution. A model of the mode of development of these peculiar rocks is reconstructed, taking into account their characters and limitations of previous interpretations. They are interpreted as transported debris deposits of syntectonogenic material released during the episodic activity of the growth faults of the Kaladgi and Vindhyanchal Basins that was diagenetically silicified.Keywords
Proterozoic, Chertbreccias, Kaladgi Basin, Vindhyanchal Basin, India.References
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