Mantle sources of kimberlites through time: A U-Pb and Lu-Hf isotope study of zircon megacrysts from the Siberian diamond fields-Reference-Cited by-同舟云学术

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Mantle sources of kimberlites through time: A U-Pb and Lu-Hf isotope study of zircon megacrysts from the Siberian diamond fields

Published:2018-02 Issue: Volume:479 Page:228-240
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Sun Jing,Tappe Sebastian,Kostrovitsky Sergey I.,Liu Chuan-Zhou,Skuzovatov Sergey Yu.,Wu Fu-Yuan

Funder

National Natural Science Foundation of China

China University of Petroleum, Beijing

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference97 articles.

1. U-Pb age and origin of gem zircon from the New England sapphire fields, New South Wales, Australia;Abduriyim;Aust. J. Earth Sci.,2012

2. Metasomatism in lithospheric mantle roots: constraints from whole-rock and mineral chemical composition of deformed peridotite xenoliths from kimberlite pipe Udachnaya;Agashev;Lithos,2013

3. Correction of common lead in U-Pb analyses that do not report 204Pb;Andersen;Chem. Geol.,2002

4. High-He3 plume origin and temporal-spatial evolution of the Siberian flood basalts;Basu;Science,1995

5. Trace element composition and cathodoluminescence properties of southern African kimberlitic zircons;Belousova;Min. Mag.,1998

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