Low δ18O magmas in the carboniferous intra-oceanic arc, central Tibet: Implications for felsic magma generation and oceanic arc accretion-Reference-Cited by-同舟云学术

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Low δ18O magmas in the carboniferous intra-oceanic arc, central Tibet: Implications for felsic magma generation and oceanic arc accretion

Published:2019-02 Issue: Volume:326-327 Page:28-38
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Dan Wei,Wang Qiang,Li Xian-Hua,Tang Gong-Jian,Zhang Chunfu,Zhang Xiu-Zheng,Wang Jun

Funder

National Key R & D Program of China

Key Program of the Chinese Academy of Sciences

Strategic Priority Research Program (A) of the Chinese Academy of Sciences

National Natural Science Foundation of China

GIGCAS 135

Key Program of Guangzhou City

GIGCAS

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference90 articles.

1. Low-O-18 silicic magmas, why are they so rare?;Balsley;Earth Planet. Sci. Lett.,1998

2. Geochemistry and Petrogenesis of Silicic Magmas in the Intra-Oceanic Kermadec Arc;Barker;J. Petrol.,2013

3. Dehydration melting and water-saturated melting of basaltic and andesitic greenstones and amphibolites at 1, 3, and 6.9kb;Beard;J. Petrol.,1991

4. Oxygen Isotopes in Mantle and Crustal Magmas as Revealed by Single Crystal Analysis. Minerals, Inclusions and Volcanic Processes 69;Bindeman,2008

5. Origin and evolution of silicic magmatism at yellowstone based on Ion microprobe analysis of isotopically zoned zircons;Bindeman;J. Petrol.,2008

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