Re–Pt–Os Isotopic and Highly Siderophile Element Behavior in Oceanic and Continental Mantle Tectonites-Reference-Cited by-同舟云学术

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Re–Pt–Os Isotopic and Highly Siderophile Element Behavior in Oceanic and Continental Mantle Tectonites

Published:2015-12-14 Issue:1 Volume:81 Page:369-440
ISSN:1529-6466
Container-title:Reviews in Mineralogy and Geochemistry
language:en
Short-container-title:Reviews in Mineralogy and Geochemistry

Author:

Becker Harry,Dale Christopher W.

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology

Cited by 61 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Evidence for large-scale, long-term highly siderophile element heterogeneities in the Atlantic mantle from Leg 153 and 209 peridotites;Geochimica et Cosmochimica Acta;2024-08

2. Sources of Ore Material in the Platinum-Group Element Deposits of Polar Siberia and the Middle Urals Based on the Data from Radiogenic (Re–Os, Pt–Os) and Stable (Cu, S) Isotopes;Russian Geology and Geophysics;2024-03-01

3. Highly siderophile element abundances and ¹⁸⁷Re‐¹⁸⁷Os systematics in the Tafassasset carbonaceous‐like primitive achondrite;Meteoritics & Planetary Science;2024-02-19

4. Eoarchean ultramafic rocks represent crustal cumulates: A case study of the Narssaq ultramafic body, southern West Greenland;Earth and Planetary Science Letters;2024-01

5. Continental lithospheric mantle;Reference Module in Earth Systems and Environmental Sciences;2024

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