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Fotedar, B. K.
- Petrography and Geochemistry of the Sandstones of Murree Group Around Laren, Udhampur, Jammu Himalaya
Abstract Views :172 |
PDF Views:2
Authors
Affiliations
1 Post Graduate Department of Geology, Jammu University, Jammu, IN
1 Post Graduate Department of Geology, Jammu University, Jammu, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 36, No 5 (1990), Pagination: 502-511Abstract
The importance of the sandstones of Murree Group is becoming more and more due to the possibilities of occurrence of hydrocarbons. It is evident from the petrographic and geochemical studies that these sandstones are of sublitharenite type. Probably low to medium grade metamorphic, intermediate to acid igneous and preexisting sedimentary rocks were sources for these rocks. A cratonic near-shore depositional environment is suggested for these sediments. The palaeoclimatic conditions were mild as indicated by their mineralogy.Keywords
Petrology (Sedimentary), Geochemistry, Sandstone, Murree Group, Jammu, Kashmir Himalaya.- A Petrochemical Study of the Gabbroic Rocks of Warikwah, Baramulla District, Kashmir Himalaya
Abstract Views :200 |
PDF Views:1
Authors
B. K. Fotedar
1,
A. K. Raina
2
Affiliations
1 Post-Graduate Department of Geology, Jammu University, Jammu - 180004
2 Post-Graduate Department of Geology, Jammu University, Jammu - 180004, IN
1 Post-Graduate Department of Geology, Jammu University, Jammu - 180004
2 Post-Graduate Department of Geology, Jammu University, Jammu - 180004, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 43, No 4 (1994), Pagination: 371-379Abstract
A gabbroic pluton of 4 sq km areal extension crops out at Warikwah, Baramulla District, Kashmir Himalaya. The three rock types in the pluton are recognized as norite, gabbro and quartz gabbro which are the products of differentiation under low PH2O conditions in that order. The parental magma is considered to be of tholeiitic nature and is derived from a deep source as reflected by major and trace element variation. After the emplacement in an orogenic (collisional) tectonic setting, the pluton has undergone low-grade. amphibolite facies metamorphism.Keywords
Gabbro, Petrochemistry, Warikwah, Baramulla District, Kashmir Himalaya, Jammu and Kashmir.- Geological and Structural Features of Gulabgarh Area, Kashmir Himalaya with a Brief Note on the Study of Associated Granitoids
Abstract Views :197 |
PDF Views:1
Authors
A. K. Koul
1,
B. K. Fotedar
2
Affiliations
1 Department of Geology, Govt Degree College, Kathua, IN
2 Post Graduate Department of Geology, Jammu University, Jammu, IN
1 Department of Geology, Govt Degree College, Kathua, IN
2 Post Graduate Department of Geology, Jammu University, Jammu, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 44, No 4 (1994), Pagination: 381-390Abstract
The Gulabgarh region of Kashmir Himalaya presents an interesting area in providing the complete geological section from Salkhalas to Tertiaries which are traversed by two tectonic planes viz., the Murree Thrust in the south and the Panjal Thrust in the north. An attempt has been made in this paper to present pragmatic classificatory models of granites after comparing the tectonic groups of the present area with the classic areas elsewhere in the world.Keywords
Sructural Geology, Granites,Tanawal Formation, Salkhala Group, Jammu and Kashmir.- Geology in School Education
Abstract Views :177 |
PDF Views:121
Authors
Affiliations
1 Jammu, IN
1 Jammu, IN