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Sharma, R. P.
- Structural Study in the Sorphatak Area, District Almora U.P. (A Part of the Almora Nappe)
Abstract Views :202 |
PDF Views:128
Authors
Affiliations
1 Department of Geology, University of Lucknow, Lucknow, IN
1 Department of Geology, University of Lucknow, Lucknow, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 12, No 4 (1971), Pagination: 387-392Abstract
No Abstract.- Geology of Devidhura Area, Almora, U.P.
Abstract Views :418 |
PDF Views:3
Authors
R. C. Misra
1,
R. P. Sharma
1
Affiliations
1 Department of Geology, University of Lucknow, Lucknow, IN
1 Department of Geology, University of Lucknow, Lucknow, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 8 (1967), Pagination: 110-118Abstract
The area around the village Devidhura (79°52'22" : 29°25'30") covering about 250 square miles forms the subject matter of the present study. Two major tectonic units-the Almora nappe and the Krol nappe-separated by the Ladhiya Thrust can be recognized in the area. Crystallines corresponding to the Almora nappe have been thrusted over the sedimentary quartzites (resembling Nagthats) of the Krol nappe.- Simla Group - A Reclassification of the 'Chail Series' 'Jaunsar Series' and 'Simla Slates' in the Simla Himalaya
Abstract Views :234 |
PDF Views:4
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 :168 |
PDF Views:119
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.- Superposed Folding in the Lower Vindhyans of Dala-Gurma Area, Mirzapur District
Abstract Views :177 |
PDF Views:2
Authors
Affiliations
1 Department of Geology, Lucknow University, Lucknow, IN
1 Department of Geology, Lucknow University, Lucknow, IN