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Rajagopalan Nair, S.
- Post-Kurnool Thrust and other Structural Features in the Northeast Part of the Palnad Basin, Krishna District, Andhra Pradesh
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Authors
Affiliations
1 Geological Survey of India, Andhra Pradesh Circle (N), Hyderabad 500029, IN
1 Geological Survey of India, Andhra Pradesh Circle (N), Hyderabad 500029, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 18, No 3 (1977), Pagination: 111-116Abstract
In the northeast part of the Palnad Basin, Krishna district, Andhra Pradesh, interesting structural features are noticed in Precambrian sedimentary rocks. A prominent thrust which has brought the Cumbums over the younger Kurnools, and other primary and secondary structures in the rocks are significant and help in deciphering structural events. The thickness of the Narji limestones based on the structural studies is estimated to be 300 m and not 6400 m as suggested by Heron.- Stratigraphy of the Upper Precambrian Albaka Belt, East of the Godavari River in Andhra Pradesh and Madhya Pradesh
Abstract Views :190 |
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Authors
Affiliations
1 6-3-628/8/1, Ravindra Nagar, Khairatabad, Hyderabad 500004, IN
2 Barkatpura, Hyderabad, IN
3 Ananda Nagar, Khairatabad, Hyderabad 500004, IN
1 6-3-628/8/1, Ravindra Nagar, Khairatabad, Hyderabad 500004, IN
2 Barkatpura, Hyderabad, IN
3 Ananda Nagar, Khairatabad, Hyderabad 500004, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 20, No 5 (1979), Pagination: 205-213Abstract
The lithostratigraphic succession worked out for the Upper Precambrian of Venkatapuram-Cherla area includes Cherla Formation, Somandevara Quartzite, Tippapuram Shale Utlapalli Conglomerate, Albaka Sandstone, Nambi Breccia and Doli and Usur Sandstones. Three disconformities, one each at the base of the Somandevara Quartzite, Utlapalli Conglomerate and the Nambi Breccia, have been inferred. Of these, the one at the base of the Nambi is believed to be the most significant one. Based on gross lithological similarity and relative stratigraphic position, the different Upper Precambrian units of this area are correlated with those of the already established Pakhal and Sullavai Groups of the main Upper Precambrian belt, west of the Godavari River. The correlation implies that the nature of the contact between the Pakhal and Sullavai Groups of the, main Upper Precambrian belt on the western side of the Godavari, a much debated question, is a profound unconformity.- Laterite Cappings in Parts of Medak and Nizamabad Districts, Andhra Pradesh
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PDF Views:118
Authors
Affiliations
1 3-4-756 A/I, Barkatpura, Hyderabad, IN
2 10-2-317/22, Vijayanagar Colony, Hyderabad, IN
3 12-2-111/A, Muradnagar, Mehdipatnam, Hyderabad, IN
4 3-4-448,2/1, Narayanguda, Hyderabad, IN
1 3-4-756 A/I, Barkatpura, Hyderabad, IN
2 10-2-317/22, Vijayanagar Colony, Hyderabad, IN
3 12-2-111/A, Muradnagar, Mehdipatnam, Hyderabad, IN
4 3-4-448,2/1, Narayanguda, Hyderabad, IN