Andesitic arc magmas derived from two contrasting mélange origins: Evidence from central Tibetan dioritic porphyries-Reference-Cited by-同舟云学术

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Andesitic arc magmas derived from two contrasting mélange origins: Evidence from central Tibetan dioritic porphyries

Published:2024-04 Issue: Volume:650 Page:121920
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Hao Lu-Lu,Wang Qiang,Kerr Andrew C.,Huang Fang,Xiao Ming,Ma Xiao-Long,Zhang Wan-Feng,Wang Wen-Yu,Liu Mao-Rui

Funder

National Natural Science Foundation of China

Youth Innovation Promotion Association of the Chinese Academy of Sciences

Publisher

Elsevier BV

Reference48 articles.

1. Diapirs as the source of the sediment signature in arc lavas;Behn;Nat. Geosci.,2011

2. A non-basaltic experimental cotectic array for calc-alkaline batholiths;Castro;Lithos,2021

3. Melting relations of MORB-sediment mélanges in underplated mantle wedge plumes: implications for the origin of Cordilleran-type batholiths;Castro;J. Petrol.,2010

4. Petrology and SHRIMP UePb zircon geochronology of Cordilleran granitoids of the Bariloche area, Argentina;Castro;J. S. Am. Earth Sci.,2011

5. Generation of new continental crust by sublithospheric silicic-magma relamination in arcs: a test of Taylor’s andesite model;Castro;Gondwana Res.,2013

Cited by 1 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Tin isotope heterogeneity and baseline of the upper continental crust;Geochimica et Cosmochimica Acta;2024-09

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