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Kumar, Gopendra

• Cambrian Trace Fossils from the Spiti Valley, Himachal Himalaya

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Authors

O. N. Bhargava ¹, Gopendra Kumar ², S. S. Gupta ³

Affiliations
1 529, Sector 18B, Chandigarh 160 018, IN
2 47, Pandariba, Lucknow 226 001, IN
3 Gandhi Nagar, Jammu 180 001, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 23, No 4 (1982), Pagination: 183-191

Abstract

Trace fossils Diplichnites spp., ? Dimorphichnus, Monomorphichnus spp., trilobite scratch marks, Gyrochorte, Gordia, ? Astropolithon, ? Scolicia, Planolites, Skolithos are reported from the Kunzam La Formation of the Haimanta Group of the Parahio section, Spiti valley. This fossil assemblage occurs 460m below the Middle Cambrian trilobite zone and 1620 m above Precambrian-Cambrian acritarch zone and may represent late Lower to Early Middle Cambrian age. These occur in sediments laid in a low energy environment.

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• Bolaspidella from the Cambrian of Kashmir and its Stratigraphic Significance

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Authors

Gopendra Kumar ¹

Affiliations
1 Geological Survey of India B-ll, H. Road, Mahanagar Extension, Lucknow-226 006, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 24, No 8 (1983), Pagination: 430-430

Abstract

No Abstract.

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• Comment

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Authors

Gopendra Kumar ¹, D. K. Bhatt ¹

Affiliations
1 Geological Survey of India, Luck now 226006, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 4 (1985), Pagination: 290-291

Abstract

No Abstract.

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• Trace Fossils from Cambrian Tal Formation, Himachal Lesser Himalaya, India, and their Stratigraphic Significance

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Authors

V. K. Mathur ¹, Ashutosh Joshi ¹, Gopendra Kumar ¹

Affiliations
1 Himalayan Geology Division, Geological Survey of India, Sector E, Aliganj, Lucknow 226 020, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 31, No 5 (1988), Pagination: 467-475

Abstract

Two assemblages of ichnofossils are recorded from the Cambrian Tal Formation, Nigalidhar Syncline, Himachal Lesser Himalaya. The assemblage-I. occurring in the Arenaceous Member 300m below the horizon yielding redlichiid trilobite and brachiopod faunas of Tsanglangpuian Stage of Early Cambrian, contains forms like Rusophycus sp. aff. R. carinata Seilacher, monomorphichnus lineatus Crimes, Diplichnites spp.) Gordia sp., Astropolichon sp., ichnogenus A and ichnogenus B. The assemblage-II, in the Phulchatti Member ('Upper Tal'), includes Cruziana sp. and ichnogenus C cf. Buthotrephis. It occurs in sediments 70 m above the horizon containing trilobites and brachiopods. The former assemblage is of world-wide distribution in Lower Cambrian (upper Meishucunian to Lower Qiongzhusian), and thus, in the absence of microfauna, can be utilised in identifying Early Cambrian successions.

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• Note on 'Record of Ediacaran Fauna from India'

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Authors

Gopendra Kumar ¹

Affiliations
1 Geol. Survey of lndia, Itanagar 791111, Arunachal Pradesh, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 34, No 6 (1989), Pagination: 669-670

Abstract

No Abstract.

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• First Report of Dasycladacean Alga - Cyclocrinites from the Ordovician of Takche Formation, Spiti, India

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Authors

P. K. Maithy ¹, Amit K. Ghosh ¹, Gopendra Kumar ²

Affiliations
1 Birbal Sahni institute of Palaeobotany, 53 University Road, Lucknow - 226 007, IN
2 48 Pandariba, Old Kanpur Road, Lucknow - 226 004, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 54, No 4 (1999), Pagination: 379-385

Abstract

Paper deals with the first occurrence of cyclocrinitids, belonging to an extinct tribe of dasycladacean algae from the Ordovician of Takche Formation Spiti Valley, Himachal Pradesh, India. Cyclocrinites favus and Cyclocrinites pyriformis are described here for the first time from the Ordovician of India and their stratigraphic significance and palaeoecological implications discussed.

Keywords

Palaeoecology, Ordovician, Stratigraphy, Cyclocrinitids, Taxonomy, Spiti, Himachal Pradesh.

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• Three-Phased Temporal Evolution of the Jhirgadandi Granite Complex, Sonbhadra District, Uttar Pradesh

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Authors

Anand Kumar Srivastava ¹, Gopendra Kumar ², D. Bhattacharya ³

Affiliations
1 Department of Geology, Lucknow University, Lucknow, IN
2 48 Pandariba, Lucknow - 226 004, IN
3 AMD/DAE, NR, West Block - 7, R K Puram, New Delhi - 110 066, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 72, No 2 (2008), Pagination: 281-282

Abstract

No Abstract.

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• Some Examples of Flame Structures from Garbyang Paleolake, Kumaun Tethys Himalaya

Abstract Views :176  |  PDF Views:133

Authors

Gopendra Kumar ¹

Affiliations
1 48, Pandariba, Behind UPSRTC Bus Station, Charbagh, Lucknow - 226 004, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 70, No 4 (2007), Pagination: 679-680

Abstract

No Abstract.

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• Obruchevella and Other Terminal Proterozoic (Vendian) Organic Walled Microfossils from the Bhander Group (Vindhyan Supergroup), Madhya Pradesh

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Authors

P. K. Maithy ¹, Gopendra Kumar ², Bijai Prasad ³

Affiliations
1 Birbal Sahani Institute of Paleobotany, Lucknow, IN
2 Geological Survey of India, Lucknow, IN
3 ONGC Ltd., Dehradun, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 70, No 2 (2007), Pagination: 373-375

Abstract

No Abstract.

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• Lower Gondwana Plant Fossils from Arunachal Lesser Himalaya and their Age

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Authors

P. K. Maithy ¹, C. M. Bindal ², S. K. Bhushan ³, Subodh Sharma ⁴, D. C. Banerji ⁵, Gopendra Kumar ⁶

Affiliations
1 F2212, Rajajipuram, Lucknow, IN
2 Geological Survey of India Lucknow, IN
3 Geological Survey of India Kolkota
4 Geological Survey of India Nagpur, IN
5 Geological Survey of India Jabalpur, IN
6 Geological Survey of India 48 Pandariba, Lucknow - 226 004, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 68, No 2 (2006), Pagination: 316-326

Abstract

Lower Gondwana plant fossils from the Bharell Formation, exposed between Plnjoll Nala and Sessa along the Bhalukpong - Bomdila Road, West Kameng district Arunachal Pradesh, are described and reviewed The assemblage comprises Gangarnopteris cyclopterozdes, G intermedia, Glossopteris angustifolra, G communls, G damudIca, G indica, G lntennlttens, Scutum cf stowanum, Vertebrarra indica, Noeggerathiopsis sp , Cherrophyllum lacerata, stem of Buriadia, Cordaicarpus cordal, Rotundocarpus strlatus and Walzkalia cahenu The assemblage is comparable to that of the Karharbari Formation of Early Permian Coalfields of Peninsular India.

Keywords

Plant Fossils, Karharbari, Early Perimian, Arunachal Hlmalaya.

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• GSSP for Terminal Proterozoic and Formal Naming of the Ediacaran System

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Authors

Gopendra Kumar ¹

Affiliations
1 48, Pandariba, Behind Charbagh Bus Station, Lucknow - 226 004, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 64, No 2 (2004), Pagination: 238-238

Abstract

No Abstract.

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