Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Benjamin Z. Klein"'
Autor:
Benjamin Z. Klein, Mark D. Behn
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 11, Pp n/a-n/a (2021)
Abstract At subduction zones, significant volumes of sediments and other crustal material are carried on top of the downgoing plate past the trench and into the mantle. This represents the dominant process by which material from the Earth's surface i
Externí odkaz:
https://doaj.org/article/b646f3f430c44563b92bdd1f03afec67
Publikováno v:
Geochemistry, Geophysics, Geosystems, 24 (5)
During the differentiation of arc magmas, fractionating liquids follow a series of cotectics, where the co-crystallization of multiple minerals control the melt compositional trajectories, commonly referred to as liquid lines of descent (LLD). These
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c5ac490199051186d8eca1f9441770d
https://hdl.handle.net/20.500.11850/615078
https://hdl.handle.net/20.500.11850/615078
Autor:
Benjamin Z. Klein, Michael P. Eddy
Publikováno v:
Geological Society of America Bulletin.
Accurate assessment of the duration of zircon crystallization within igneous rocks is critical for constraining the time scales of magmatic evolution and storage, which have important implications for our understanding of magmatic fluxes and volcanic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5212cadf0f83c77580c6f592b5c5026
https://doi.org/10.1130/b36686.1
https://doi.org/10.1130/b36686.1
Publikováno v:
Geology. 49:106-110
The Bear Valley Intrusive Suite (BVIS), located in the southernmost Sierra Nevada Batholith (SNB; California, USA) exposes a transcrustal magma system consisting of lower-crustal gabbros and volumetrically extensive middle- and upper-crustal tonalite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c1daafb2d6fa0538bf57964ec4bc25d
https://doi.org/10.1130/g47952.1
https://doi.org/10.1130/g47952.1
Publikováno v:
Springer Berlin Heidelberg
Exposures of arc crustal sections represent rare opportunities to directly evaluate lower crustal magmatic processes and their link to arc products in the middle and upper crust. Within the southernmost Sierra Nevada batholith, the Bear Valley Intrus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a32caa65769a08c5193088323153d62
https://doi.org/10.1007/s00410-021-01832-2
https://doi.org/10.1007/s00410-021-01832-2
Publikováno v:
Goldschmidt2021 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43597be081f0aefd83c6b26af832c180
https://doi.org/10.7185/gold2021.8120
https://doi.org/10.7185/gold2021.8120
Autor:
Benjamin Z. Klein, Oliver Jagoutz
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3893cc3e9ce59d5e52aa387f80931a76
https://doi.org/10.1130/abs/2020am-358982
https://doi.org/10.1130/abs/2020am-358982
Autor:
Benjamin Z. Klein, Mark D. Behn
Publikováno v:
Goldschmidt Abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcce43b489f2c7963aa03d952343f8cc
https://doi.org/10.46427/gold2020.1332
https://doi.org/10.46427/gold2020.1332
Autor:
Benjamin Z. Klein, Oliver Jagoutz
Publikováno v:
American Journal of Science. 318:29-63
In this paper we review processes responsible for the formation of granites in subduction systems. While there is robust evidence that strongly peraluminous, so-called S-type granites are formed by melting of metasediments in the (lower) crust, the p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78c607613870c96c468b261e7851fb3e
https://doi.org/10.2475/01.2018.03
https://doi.org/10.2475/01.2018.03
Publikováno v:
Earth and Planetary Science Letters. 474:516-526
Higher mantle potential temperatures characterized the early Earth, resulting in thicker, more mafic oceanic crust entering subduction systems. This change in the composition of subducted slabs, combined with the enhanced temperature contrast between
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d139932090ecf8b91401ddb0c96ff9c
https://doi.org/10.1016/j.epsl.2017.07.003
https://doi.org/10.1016/j.epsl.2017.07.003