Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe-Reference-Cited by-同舟云学术

Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe

Published:2019-04 Issue:4 Volume:124 Page:3588-3604
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Huang Jian¹²^ORCID,Ackerman Lukáš³,Zhang Xing‐Chao¹,Huang Fang¹²^ORCID

Affiliation:

1. CAS Key Laboratory of Crust‐Mantle Materials and Environments, School of Earth and Space Sciences University of Science and Technology of China Hefei China

2. CAS Center for Excellence in Comparative Planetology China

3. Institute of Geology of the Czech Academy of Sciences Prague Czech Republic

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017125

Reference100 articles.

1. Re–Os and Lu–Hf isotopic constraints on the formation and age of mantle pyroxenites from the Bohemian Massif