Zobrazeno 1 - 10
of 46
pro vyhledávání: '"Stein B."'
Publikováno v:
Earth and Planetary Science Letters. 594:117743
Autor:
Sarah T. Stewart, Dayne Fratanduono, Marius Millot, B. Chidester, E. J. Davies, Seth Root, Joshua P. Townsend, P. Kalita, Stein B. Jacobsen, D. K. Spaulding
Publikováno v:
Geophysical Research Letters. 48
Autor:
D. K. Spaulding, Stein B. Jacobsen, Seth Root, E. J. Davies, M. S. Duncan, R. G. Kraus, Sarah T. Stewart
Publikováno v:
Journal of Geophysical Research. Planets
The physical processes during planet formation span a large range of pressures and temperatures. Giant impacts, such as the one that formed the Moon, achieve peak pressures of 100s of GPa. The peak shock states generate sufficient entropy such that s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bb688269c82d695ff5c22842dbf10bf9
https://hdl.handle.net/10919/104456
https://hdl.handle.net/10919/104456
Autor:
Stein B. Jacobsen, Yongsheng He, Rosalind Tuthill Helz, Shichun Huang, Bruce D. Marsh, Fang-Zhen Teng, Hongming Zhang, Yang Wang
Publikováno v:
Geochemistry, Geophysics, Geosystems. 19:3128-3139
Publikováno v:
Earth and Planetary Science Letters. 578:117291
In subduction zones, fluids rise from the slab to the mantle, causing metasomatism and flux melting of the mantle to produce arc magmas. The transfer of material from slab to mantle and, in turn, to arc crust is an important control on the long-term
Autor:
E. J. Davies, Seth Root, Stein B. Jacobsen, Richard Kraus, Dylan Spaulding, Philip J. Carter, Sarah T. Stewart
Collisions that induce melting and vaporization can have a substantial effect on the thermal and geochemical evolution of planets. However, the thermodynamics of major minerals are not well known at the extreme conditions attained during planet forma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::989b41187e09f031e5b02884acdaf2a1
Publikováno v:
Earth and Planetary Science Letters. 440:158-168
The upper mantle is widely accepted to be pyrolitic, but the bulk composition of the lower mantle remains highly disputed. Recent modeling of the lower mantle shear wave velocity profile has suggested that the lower mantle is enriched in bridgmanite,
Publikováno v:
Earth and Planetary Science Letters. 430:202-208
Recent high-precision isotopic measurements show that the isotopic similarity of Earth and Moon is unique among all known planetary bodies in our Solar System. These observations provide fundamental constraints on the origin of Earth–Moon system, l
Autor:
Rolf L. Romer, Fang-Zhen Teng, Wei Yang, Wang-Ye Li, Shan Ke, Clemens V. Ullmann, Fatemeh Sedaghatpour, Philip A.E. Pogge von Strandmann, Stein B. Jacobsen, Qing-Zhu Yin, Uwe Wiechert, Anette Meixner, Joshua Wimpenny, Ramananda Chakrabarti
Publikováno v:
Geochemistry, Geophysics, Geosystems. 16:3197-3209
To evaluate the interlaboratory mass bias for high-precision stable Mg isotopic analysis of natural materials, a suite of silicate standards ranging in composition from felsic to ultramafic were analyzed in five laboratories by using three types of m
Autor:
E. J. Davies, David E. Bliss, Marius Millot, Stein B. Jacobsen, Dayne Fratanduono, Luke Shulenburger, D. K. Spaulding, Seth Root, Sarah T. Stewart, Richard Kraus, Joshua P. Townsend, Raymond W. Lemke
Publikováno v:
Root, Seth; Townsend, Joshua P; Davies, Erik; Lemke, Raymond W; Bliss, David E; Fratanduono, Dayne E; et al.(2018). The Principal Hugoniot of Forsterite to 950 GPa. Geophysical Research Letters, 45(9), 3865-3872. doi: 10.1029/2017GL076931. UC Office of the President: UC Lab Fees Research Program (LFRP); a funding opportunity through UC Research Initiatives (UCRI). Retrieved from: http://www.escholarship.org/uc/item/2c57h1qm
Author(s): Root, Seth; Townsend, Joshua P; Davies, Erik; Lemke, Raymond W; Bliss, David E; Fratanduono, Dayne E; Kraus, Richard G; Millot, Marius; Spaulding, Dylan K; Shulenburger, Luke; Stewart, Sarah T; Jacobsen, Stein B
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de4dcc6c871b6969cc7802b06ab34f80
http://www.escholarship.org/uc/item/2c57h1qm
http://www.escholarship.org/uc/item/2c57h1qm