Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Barun K. Mukherjee"'
Publikováno v:
International Journal of Earth Sciences. 110:2849-2862
Peridotites in ophiolites exposed along Himalayan suture zone open window to study deep Earth processes. We report c.2 km thick well exposed mantle section of Shergol ophiolite in the Indus Suture Zone (ISZ). The mantle section comprises lherzolite,
Publikováno v:
Current Science. 121:560
Autor:
Barun K. Mukherjee, Koushick Sen, Satadru Bhattacharya, Souvik Das, Robert T. Gregory, Franco Marcantonio, Asish R. Basu
Publikováno v:
Chemical Geology. 551:119772
Ophicarbonates are found in ophiolite-associated peridotites and bear signature of fluid-rock interaction either on ocean floor or during ophiolite emplacement. The occurrence of ophicarbonate veins hosted by ultramafic rocks of the Indus Ophiolite,
Publikováno v:
Journal of Structural Geology. 62:13-24
In the eastern part of Ladakh, the right-lateral Karakoram Fault Zone (KFZ) bifurcates into two strands called the Pangong Strand and the Tangtse Strand. These two strands bound a region called the Pangong Transpression Zone (PTZ), which consists of
Autor:
Rodolfo Carosi, Soumyajit Mukherjee, Peter van der Beek, Delores M. Robinson, Barun K. Mukherjee
Publikováno v:
Geological Society, London, Special Publications. 412:1-3
SOUMYAJIT MUKHERJEE1*, RODOLFO CAROSI2, PETER VAN DER BEEK3, BARUN KUMAR MUKHERJEE4 & DELORES M. ROBINSON5 Department of Earth Sciences, Indian Institute of Technology Bombay, Powai, Mumbai 400 076, Maharashtra, India Dipartimento di Scienze della Te
Publikováno v:
International Journal of Earth Sciences. 102:2033-2042
Zildat Ophiolitic Melange (ZOM) of the Indus Suture Zone, Himalaya, represents tectonic blocks of the fragmented oceanic metasediments and ophiolite remnants. The ZOM is sandwiched between the Zildat fault adjacent to a gneissic dome known as Tso Mor
Publikováno v:
Proceedings of Indian National Science Academy, Vol 82, Iss 3 (2016)
Status of Research in Structural Geology; the Indian Scene During the Last Five Years
The Nidar Ophiolite Complex (NOC) consists of a c. 10 km thick ophiolite suite in the NW Himalaya, India. The c. 7 km thick lower ultramafic part of the ophiolite body terminates against the Tso Morari Crystallines, which represent the leading edge o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a0cee994d03e52b70c43396570be137
Publikováno v:
Geological Society of America Abstracts with Programs.