Zobrazeno 1 - 10
of 119
pro vyhledávání: '"Fernando Bea"'
Autor:
Hisatoshi Ito, Yoshiko Adachi, Aitor Cambeses, Fernando Bea, Mayuko Fukuyama, Koji Fukuma, Ryuji Yamada, Takashi Kubo, Mami Takehara, Kenji Horie
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-14 (2021)
Abstract The Quaternary Kurobegawa Granite, central Japan, is not only the youngest known granitic pluton exposed on the Earth’s surface, it is one of few localities where both Quaternary volcanics and related plutons are well exposed. Here, we pre
Externí odkaz:
https://doaj.org/article/9f3a4073514e4e478a60e5853e4f3e8b
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-10 (2018)
Abstract Zircon of crustal origin found in mantle-derived rocks is of great interest because of the information it may provide about crust recycling and mantle dynamics. Consideration of this requires understanding of how mantle temperatures, notably
Externí odkaz:
https://doaj.org/article/0426d09772154fa1886e03154b610e9e
Publikováno v:
Литосфера, Vol 18, Iss 2, Pp 177-207 (2018)
A model of magma formation in the crust of the Urals mobile belt, which is the best example of epioceanic suprasubduction orogen, has been developed. Magma formation occurs both in the relic oceanic and in the newly formed orogen crust. In the first
Externí odkaz:
https://doaj.org/article/c3cc1aad0c70485c9930d2f0db590297
Publikováno v:
Digibug. Repositorio Institucional de la Universidad de Granada
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We are indebted to Yamirka Rojas-Agramonte, Ian Williams, and an anonymous reviewer for their constructive comments. The thorough revision and editorial handling by Sumit Chakraborty are also gratefully acknowledged. This work has been financially su
Publikováno v:
American Mineralogist. 106:782-800
The amphibole-plagioclase NaSi-CaAl exchange thermometer by Holland and Blundy (1994) (expression B) has been extensively applied to calcic amphibole-bearing assemblages from metamorphic and igneous rocks, whereas the more recent calibrations of the
Zircon derived from crustal rocks can survive dissolution into basic melt during rock assimilation and magma hybridization if shielded in mafic phenocrysts or minerals from non-disaggregated xenoliths. Under these conditions, zircon can be subject to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b69a16fb735a20884da8e968c48790b3
https://doi.org/10.5194/egusphere-egu22-1195
https://doi.org/10.5194/egusphere-egu22-1195
Publikováno v:
Earth and Planetary Science Letters. 601:117911
Autor:
Fernando Bea, Pilar Montero, Leticia Barcos, Aitor Cambeses, José Francisco Molina, Irene Morales
Publikováno v:
Lithos. :106940
Autor:
S. G. Skolotnev, N. S. Bortnikov, T. F. Zinger, Evgenii Sharkov, Fernando Bea, S. А. Silantiev, Pilar Montero
Publikováno v:
Доклады Академии наук. 489:483-489
U-Pb age, oxygen and hafnium isotopic ratios in zircon from rocks of ocean core complexes at Mid-Atlantic Ridge have been studied using SHRIMP and MC-LA-ICP-MS techniques. U-Pb dating revealed four group of zircons: 1) 0,6-1,7 Ma, 2) 6,7-11,2 Ma, 3)
Autor:
N. S. Bortnikov, Sergei Silantyev, Pilar Montero, Evgenii Sharkov, T. F. Zinger, S. G. Skolotnev, Fernando Bea
Publikováno v:
Doklady Earth Sciences. 489:1396-1401
The U–Pb age and oxygen and hafnium isotope ratios of zircon from rocks of oceanic core complexes along the Mid-Atlantic Ridge have been studied using SHRIMP and MC-LA-ICP-MS techniques. The U–Pb dating revealed four groups of zircon: (1) 0.6–1