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Dasgupta, Somnath
- Eastern Ghats Granulites
Abstract Views :106 |
PDF Views:62
Authors
Affiliations
1 Department of Geological Sciences, Jadavpur University, Calcutta - 700 032, IN
1 Department of Geological Sciences, Jadavpur University, Calcutta - 700 032, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 57, No 1 (2001), Pagination: 97-98Abstract
No Abstract.- Stratigraphy of the Penganga Group Around Adilabad, Andhra Pradesh
Abstract Views :133 |
PDF Views:2
Authors
Asru K. Chaudhuri
1,
Somnath Dasgupta
2,
Goutam Bandyopadhyay
2,
Subir Sarkar
2,
P. C. Bandyopadhyay
2,
K. Gopalan
3
Affiliations
1 Geological Studies, Unit, Indian Statistical Institute, Calcutta, IN
2 Department of Geological Sciences, Jadavpur University, Calcutta 700032, IN
3 National Geophysical Research Institute, Hyderabad, IN
1 Geological Studies, Unit, Indian Statistical Institute, Calcutta, IN
2 Department of Geological Sciences, Jadavpur University, Calcutta 700032, IN
3 National Geophysical Research Institute, Hyderabad, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 34, No 3 (1989), Pagination: 291-302Abstract
The Proterozoic sequence around Adilabad, Andhra Pradesh comprises a distinct lithostratigraphic unit of 'Group' status and has been given the name Penganga Group. The Penganga Group has been classified into three Formations which are, in order of younging, Pranhita Sandstone, Chanda Limestone and Sat Nala Shale. The sequence is dominated by limestones and shales which were deposited in relatively deep water environment and, thus, contrast sharply with the conglomerate, sandstone and shallow water limestones of the Pakhal Group. Radiometric dating of fresh glauconites from middle part of the Penganga Group gives an age of 770 ± 30 Ma. Thus, the Penganga Group is the youngest of all other Proterozoic sequences in Pranhita-Godavari Valley.- Precambrian Geodynamics
Abstract Views :147 |
PDF Views:18
Authors
Affiliations
1 CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, IN
2 Indian Institute of Science Education and Research, Kolkata, Mohanpur, Nadia 741 246, IN
1 CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, IN
2 Indian Institute of Science Education and Research, Kolkata, Mohanpur, Nadia 741 246, IN
Source
Current Science, Vol 118, No 1 (2020), Pagination: 15-17Abstract
Understanding the geodynamic processes that underpin the formation of continents is fundamental to decoding the complex evolutionary history of the Earth and the terrestrial planets. In the Phanerozoic Eon, the paradigm of plate tectonics and Wilson-cycle processes not only constitutes a robust and unifying mechanism to explain the orogenic processes of crust formation, recycling and preservation, but also the complex interactions among the solid earth, biosphere, hydrosphere and atmosphere relevant to evolution of life and climate. However, there is yet no consensus on a global geodynamic framework for the Hadean and Archean Eons.- Teaching Earth science – past experience and the way forward
Abstract Views :124 |
PDF Views:18
Authors
Affiliations
1 Indian Statistical Institute, Kolkata 700 108, India and Indian Institute of Science Education and Research, Kolkata 741 246, India, IN
1 Indian Statistical Institute, Kolkata 700 108, India and Indian Institute of Science Education and Research, Kolkata 741 246, India, IN