The source and ore-forming processes of post-collisional Qulong porphyry Cu-Mo deposit in Tibet constrained by Mo isotopes-Reference-Cited by-同舟云学术

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The source and ore-forming processes of post-collisional Qulong porphyry Cu-Mo deposit in Tibet constrained by Mo isotopes

Published:2024-05 Issue: Volume:652 Page:122025
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Xue Qiqi,Zhang Lipeng,Chen Shuo,Li Congying,Li Tao,Sun Weidong

Funder

Laoshan Laboratory

National Natural Science Foundation of China

Chinese Academy of Sciences Youth Innovation Promotion Association

Taishan Scholar Foundation of Shandong Province

Publisher

Elsevier BV

Reference70 articles.

1. The isotopic signature of the global riverine molybdenum flux and anoxia in the ancient oceans;Archer;Nat. Geosci.,2008

2. Fluid-melt Mo isotope fractionation: implications for the δ98/95Mo of the upper crust;Bezard;Geochem. Perspect. Lett.,2023

3. The effects of magmatic processes and crustal recycling on the molybdenum stable isotopic composition of Mid-Ocean Ridge Basalts;Bezard;Earth Planet. Sci. Lett.,2016

4. Evidence for Mo isotope fractionation in the solar nebula and during planetary differentiation;Burkhardt;Earth Planet. Sci. Lett.,2014

5. Simple and cost-effective methods for precise analysis of trace element abundances in geological materials with ICP-MS;Chen;Sci. Bull.,2017

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