Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Anubhooti Saxena"'
Autor:
Navin Goyal, Himadri Basu, Chanchal Sarbajna, Anubhooti Saxena, Adwait Ranjan Nayak, Pritam Karmakar, T. S. Sunil Kumar
Publikováno v:
Journal of the Geological Society of India. 98:1058-1067
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9966ac20ccd032ff6fca485f0c8a666f
https://doi.org/10.1007/s12594-022-2124-9
https://doi.org/10.1007/s12594-022-2124-9
Publikováno v:
Journal of the Geological Society of India. 98:1074-1084
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07b02bcc72682999387a3210c3cfb516
https://doi.org/10.1007/s12594-022-2126-7
https://doi.org/10.1007/s12594-022-2126-7
Autor:
Anubhooti Saxena, Atanu Banerjee, Nabanita Mitra, D. S. Couto, U. K. Pandey, B. S. Bisht, D. K. Sinha
Publikováno v:
Journal of the Geological Society of India. 98:1095-1103
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a772c9e19ea8bda6a35b0beda2004f5c
https://doi.org/10.1007/s12594-022-2128-5
https://doi.org/10.1007/s12594-022-2128-5
Publikováno v:
Journal of Earth System Science. 127
Crystallochemical data on metamict davidite from albitites and albitised rocks from the Bichun area (Jaipur district, Rajasthan, India) of Banded Gneissic Complex (BGC) are provided. Davidite occurs as euhedral, subhedral to anhedral crystals in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94ac14d9f07c8cbd9a882e9d0d6e457b
https://doi.org/10.1007/s12040-017-0905-0
https://doi.org/10.1007/s12040-017-0905-0
Publikováno v:
Journal of the Geological Society of India. 82:509-518
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 Cen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9bf52842be63d97f04ba7c5bfb6c894
https://doi.org/10.1007/s12594-013-0182-8
https://doi.org/10.1007/s12594-013-0182-8
Publikováno v:
Journal of Earth System Science. 121:29-44
The Malari Leucogranite in the Garhwal Himalaya is cut across by a continental-scale normal fault system called the South Tibetan Detachment (STD). A mineralogical, geochemical and fluid inclusion study of samples from the fault zone of the Malari Gr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf841568ee198f25d6a512abc24a6299
https://doi.org/10.1007/s12040-012-0145-2
https://doi.org/10.1007/s12040-012-0145-2
Publikováno v:
Journal of Asian Earth Sciences. 41:344-354
The Greater Himalayan Sequence in the Garhwal Region of India is a 14–20 km thick succession of various pelitic and psammitic metasediments which contain individual units that are traceable for at least 250 km along the strike of the Himalayan rang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e9084d9ea27a971d71e93f6c40c364b
https://doi.org/10.1016/j.jseaes.2011.02.001
https://doi.org/10.1016/j.jseaes.2011.02.001
The Malari leucogranite, Garhwal Himalaya, northern India: Chemistry, age, and tectonic implications
Publikováno v:
Geological Society of America Bulletin. 122:1865-1876
In the Garhwal region, India, the Malari leucogranite cuts the South Tibetan detachment system, a large-scale normal fault system at the top of the High Himalaya. The leucogranite crosscuts ductile normal-sense shear fabrics and has experienced relat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::697c6ca506442d46987e7c614bc59087
https://doi.org/10.1130/b30153.1
https://doi.org/10.1130/b30153.1
