Zobrazeno 1 - 10
of 29
pro vyhledávání: '"David Hernández‐Uribe"'
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Abstract Archean (4.0–2.5 Ga) tonalite–trondhjemite–granodiorite (TTG) terranes represent fragments of Earth’s first continents that formed via high-grade metamorphism and partial melting of hydrated basaltic crust. While a range of geodynami
Externí odkaz:
https://doaj.org/article/3889d110786b47dda127f9f97a228dc8
Autor:
David Hernández‐Uribe, Chris G. Mattinson, Megan E. Regel, Jianxin Zhang, Katie A. Stubbs, Andrew R. C. Kylander‐Clark
Publikováno v:
Journal of Metamorphic Geology. 41:557-581
Autor:
Xin Chen, Shaoyong Jiang, Martin R.Palmer, Hans-Peter Schertl, Aitor Cambeses, David Hernández-Uribe, Kuidong Zhao, Chenggui Lin, Youye Zheng
Publikováno v:
Geochimica et Cosmochimica Acta. 340:120-140
Publikováno v:
Geology.
Lawsonite eclogites are major hosts of H2O and trace elements and thus key for long-term deep element cycling in subduction zones. Existing cycling models suggest that the subducting oceanic crust transforms to lawsonite-eclogite assemblages; yet the
Materials and methods for petrological modeling.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c2f3bc5aad0ef81bbee49e87cb3a0b3
https://doi.org/10.1130/geol.s.22790213
https://doi.org/10.1130/geol.s.22790213
Autor:
Emma Hart, David Hernández-Uribe, Xin Chen, Hans-Peter Schertl, Youye Zheng, Aitor Cambeses, Jarosław Majka
Publikováno v:
Geochimica et Cosmochimica Acta. 319:271-295
The behavior of Ti-Nb-Ta is crucial to reveal the genesis of island arc magmatism. However, mobilization and fractionation of Ti-Nb-Ta in subduction zone settings remain poorly understood. The discovery of felsic veins rich in coarse-grained rutile w
Autor:
Shan‐Shan Li, Kun‐Feng Qiu, David Hernández‐Uribe, Yi‐Xue Gao, M. Santosh, Hao‐Chong Huang, Zhi‐Yuan Zheng, Zi‐Li Zhang, Shi‐Chen Gao
Publikováno v:
Journal of Geophysical Research: Solid Earth. 128
Phase equilibria modeling is a powerful petrological tool to address both forward and inverse geological problems over a broad range of crustal and upper mantle conditions of pressure (P), temperature (T), composition (X), and redox (fO2). The develo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::afaf6817dc18630c90491205b1598161
http://hdl.handle.net/10138/347738
http://hdl.handle.net/10138/347738
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Scientific Reports
Scientific Reports
Archean (4.0–2.5 Ga) tonalite–trondhjemite–granodiorite (TTG) terranes represent fragments of Earth’s first continents that formed via high-grade metamorphism and partial melting of hydrated basaltic crust. While a range of geodynamic regimes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2c35c94ec4d070af28df7756d72767c5
https://doi.org/10.1038/s41598-021-84300-y
https://doi.org/10.1038/s41598-021-84300-y
Publikováno v:
Scientific Reports, Vol 9, Iss 1, Pp 1-10 (2019)
Scientific Reports
Scientific Reports
The causes of Cenozoic uplift of the Colorado Plateau, southwestern USA, are strongly debated, though most hypotheses acknowledge the importance of northwest-directed subduction of the Farallon oceanic plate beneath North America since c. 100 Ma. Exi