Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Jyotindra Sapkota"'
Autor:
Robert H. Smithies, Yongjun Lu, Tim E. Johnson, Christopher L. Kirkland, Kevin F. Cassidy, David C. Champion, David R. Mole, Ivan Zibra, Klaus Gessner, Jyotindra Sapkota, Matthew C. De Paoli, Marc Poujol
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-12 (2019)
Some of Earth’s earliest continental crust has been previously inferred to have formed from partial melting of hydrated mafic crust at pressures above 1.5 GPa (more than 50 km deep), pressures typically not reached in post-Archean continental crust
Externí odkaz:
https://doaj.org/article/7ec8b46796a14bc88ba5c9941ac2f6c4
Autor:
David C. Champion, Robert H. Smithies, Yongjun Lu, K.F. Cassidy, Jyotindra Sapkota, David R. Mole, Tim E. Johnson, I. Zibra, Marc Poujol, Klaus Gessner, Matthew C. De Paoli, Christopher L. Kirkland
Publikováno v:
Nature Communications
Nature Communications, Nature Publishing Group, 2019, 10 (1), pp.Art. n°5559. ⟨10.1038/s41467-019-13547-x⟩
Nature Communications, Vol 10, Iss 1, Pp 1-12 (2019)
Nature Communications, 2019, 10 (1), pp.Art. n°5559. ⟨10.1038/s41467-019-13547-x⟩
Nature Communications, Nature Publishing Group, 2019, 10 (1), pp.Art. n°5559. ⟨10.1038/s41467-019-13547-x⟩
Nature Communications, Vol 10, Iss 1, Pp 1-12 (2019)
Nature Communications, 2019, 10 (1), pp.Art. n°5559. ⟨10.1038/s41467-019-13547-x⟩
Much of the present-day volume of Earth’s continental crust had formed by the end of the Archean Eon, 2.5 billion years ago, through the conversion of basaltic (mafic) crust into sodic granite of tonalite, trondhjemite and granodiorite (TTG) compos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::278a62b85588d513c51904e61974be40
https://doi.org/10.1038/s41467-019-13547-x
https://doi.org/10.1038/s41467-019-13547-x
Publikováno v:
Geosciences Journal. 22:65-77
Multiple generations of sub-vertical and sub-horizontal foliations preserved as inclusion trails in garnet in mylonitic rocks from the hanging wall of the Main Central Thrust in the Himalayas indicate that these porphyroblasts did not rotate during t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5bdd4e8663369bb0e72317b6e5c4282f
https://doi.org/10.1007/s12303-017-0030-8
https://doi.org/10.1007/s12303-017-0030-8
Autor:
Richard James Squire, Ian H. Campbell, Patrick Hayman, Yuri Amelin, Mark J. Pawley, Jyotindra Sapkota, Raymond Alexander Fernand Cas, Ian Pegg, Nicolas Thébaud, Stephen Barnes
Publikováno v:
Precambrian Research. 270:334-368
The thick package of ∼2.7 Ga mafic and ultramafic lavas and intrusions preserved among the Neoarchean of the Kalgoorlie Terrene in Western Australia provides valuable insight into geological processes controlling the most prodigious episode of grow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f2fcbd765173d6821423b600fb3c9b7
https://doi.org/10.1016/j.precamres.2015.09.016
https://doi.org/10.1016/j.precamres.2015.09.016
Autor:
Jyotindra Sapkota, I. V. Sanislav
Publikováno v:
Tectonophysics. 587:89-106
The Kathmandu Thrust Sheet, which overlies the Lesser Himalayas along the southern part of the Main Central Thrust (MCT) and forms the leading edge of the Higher Himalayan crystalline rocks, is folded at a regional scale by the Gorkha-Kathmandu fold
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90846f950febff3dd072edd28384a9a9
https://doi.org/10.1016/j.tecto.2012.10.029
https://doi.org/10.1016/j.tecto.2012.10.029