Olivine Oxygen Isotope Evidence for Intracontinental Recycling of Delaminated Continental Crust-Reference-Cited by-同舟云学术

Olivine Oxygen Isotope Evidence for Intracontinental Recycling of Delaminated Continental Crust

Published:2018-07 Issue:7 Volume:19 Page:1913-1924
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Wang Chun‐Guang¹^ORCID,Xu Wen‐Liang¹²^ORCID,Yang De‐Bin¹,Liu Yong‐Sheng²^ORCID,Pei Fu‐Ping¹,Li Qiu‐Li³^ORCID,Zhou Qun‐Jun¹

Affiliation:

1. College of Earth Sciences Jilin University Changchun China

2. State Key Laboratory of Geological Processes and Mineral Resources China University of Geosciences Wuhan China

3. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

Funder

Ministry of Science and Technology of the People's Republic of China

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2017GC007284

Reference68 articles.

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2. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation

3. Effects of melt percolation on the Re–Os systematics of peridotites from a Paleozoic convergent plate margin

4. Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: Evidence for magmatic digestion and erosion of Pleistocene hyaloclastites

5. Oxygen isotopic composition of hydrous and anhydrous mantle peridotites

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