Fluid inclusion study of the Higher Himalayan quartzitic pelites, Garhwal Himalaya, India: Implicati...
Fluid inclusion study of the Higher Himalayan quartzitic pelites, Garhwal Himalaya, India: Implications for recrystallization history of metasediments
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India: Springer India
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English
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India: Springer India
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Quartzitic pelites forms a part of Higher Himalayan Crystalline of higher geotectonic zone in Garhwal Himalaya. Quartzitic pelites (locally known as Pandukeshwar Quartzite) in Garhwal Himalaya is sandwiched between high grade metamorphic rocks of Central Crystallines and Badrinath Formation. Fluid inclusion studies are carried out on the detrital,...
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Fluid inclusion study of the Higher Himalayan quartzitic pelites, Garhwal Himalaya, India: Implications for recrystallization history of metasediments
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TN_cdi_proquest_journals_1460841668
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_1460841668
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ISSN
0016-7622
E-ISSN
0974-6889
DOI
10.1007/s12594-013-0182-8
