Boron, carbon, oxygen and radiogenic isotope investigation of carbonatite from the Miaoya complex, central China: Evidences for late-stage REE hydrothermal event and mantle source heterogeneity-Reference-Cited by-同舟云学术

Boron, carbon, oxygen and radiogenic isotope investigation of carbonatite from the Miaoya complex, central China: Evidences for late-stage REE hydrothermal event and mantle source heterogeneity

Published:2018-12 Issue: Volume:322 Page:225-237
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Çimen O.,Kuebler C.,Monaco B.,Simonetti S.S.,Corcoran L.,Chen W.,Simonetti A.

Funder

University of Notre Dame

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference55 articles.

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4. Source of parental melts to carbonatites–critical isotopic constraints;Bell;Mineral. Petrol.,2010

5. Nd, Pb and Sr Isotopic Compositions of East African Carbonatites: evidence for Mantle Mixing and Plume Inhomogeneity;Bell;J. Petrol.,2001

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