Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Yan-Tao Hao"'
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 1, Iss , Pp - (2019)
Anhydrous, medium/coarse-grained spinel bearing mantle xenoliths from the Subei Basin, Eastern China have mineral arrangements that reflect low energy geometry. Because of clinopyroxene modal contents, they are grouped into cpx-rich lherzolites (cpx
Externí odkaz:
https://doaj.org/article/4e4dbb6f718e4779af1171b21be4582e
Autor:
Zhao-Feng Zhang, Jin-Ting Kang, Chen Zhou, Hongli Zhu, Fang Liu, Fang Huang, Yan-Tao Hao, Jing-Yi Huang
Publikováno v:
Geochimica et Cosmochimica Acta. 290:41-58
This study reports Ca-Fe isotope compositions of mineral separates in a set of peridotite xenoliths including ten lherzolites, one harzburgite, and one wehrlite from Hainan Island, south China. Iron isotope compositions show a small variation ( 2‰)
Publikováno v:
Goldschmidt2022 abstracts.
Publikováno v:
Goldschmidt2022 abstracts.
Publikováno v:
Goldschmidt2022 abstracts.
Publikováno v:
Goldschmidt Abstracts.
Autor:
István Kovács, Jia Liu, Qun-Ke Xia, Ying Ming Sheng, Yan-Tao Hao, Huan Chen, Pei Li, Xiaozhi Yang
Publikováno v:
National Science Review
Understanding the concentration and distribution of water in the Earth's mantle plays a substantial role in studying its chemical, physical and dynamic processes. After a decade of research, a comprehensive dataset of water content in upper-mantle sa
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 1, Iss, Pp-(2019)
Anhydrous, medium/coarse-grained spinel bearing mantle xenoliths from the Subei Basin, Eastern China have mineral arrangements that reflect low energy geometry. Because of clinopyroxene modal contents, they are grouped into cpx-rich lherzolites (cpx
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5335b6d3aadcbcd094eaebed176db8d6
http://hdl.handle.net/11392/2400242
http://hdl.handle.net/11392/2400242
Publikováno v:
Geology. 45:87-90
Both mantle-derived clinopyroxene and orthopyroxene are generally homogeneous in water concentration, while water content in the coexisting olivine is affected by partial or complete loss during the ascent of the hosting magma. Here, we report the fi
Publikováno v:
Lithos. 260:315-327
Metasomatism induced by melts/fluids is ubiquitous in the lithospheric mantle and can potentially modify the initial water content of the mantle. However, the preservation of correlations between H 2 O content and partial melting indices (e.g., Yb co