Formation of layered intrusion: A perspective from vanadium isotopes-Reference-Cited by-同舟云学术

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Formation of layered intrusion: A perspective from vanadium isotopes

Published:2024-10 Issue: Volume:482-483 Page:107699
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Lv Wei-Xin,Liu Meng-Shu,Cao Yonghua,Wang Christina Yan,Huang Fang,Ding Xin

Funder

National Natural Science Foundation of China

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

National Key Research and Development Program of China

Publisher

Elsevier BV

Reference49 articles.

1. Contrasting parental magma compositions for the Hongge and Panzhihua magmatic Fe–Ti–V oxide deposits, Emeishan large Igneous Province, SW China;Bai;Econ. Geol.,2014

2. Composition of the chilled marginal rocks of the Panzhihua layered intrusion, Emeishan large igneous province, Southwest China: Implications for parental magma compositions, sulfide saturation history and Fe-Ti oxide mineralization;Bai;J. Petrol.,2019

3. Calculation of equilibrium constants for isotopic exchange reactions;Bigeleisen;J. Chem. Phys.,1947

4. Iron isotopic evolution during fractional crystallization of the uppermost Bushveld complex layered mafic intrusion;Bilenker;Geochem. Geophys. Geosyst.,2017

5. Rift Valley in the Atlantic Ocean near 36°50′N: petrology and geochemistry of basaltic rocks;Bougault;Earth Planet. Sci. Lett.,1974

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