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pro vyhledávání: '"Matthew C. De Paoli"'
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