High-silica rhyolites in the terminal stage of massive Cretaceous volcanism, SE China: Modified crustal sources and low-pressure magma chamber-Reference-Cited by-同舟云学术

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High-silica rhyolites in the terminal stage of massive Cretaceous volcanism, SE China: Modified crustal sources and low-pressure magma chamber

Published:2020-10 Issue: Volume: Page:
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Li Xi-Yao,Li Sanzhong,Suo Yanhui,Huang Feng,Wang Pengcheng,Luan Shaorong,Zhou Jie

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Polit National Laboratory for Marine Science and Technology

Publisher

Elsevier BV

Subject

Geology

Reference108 articles.

1. Rhyolites and their source mushes across tectonic settings;Bachmann;J. Petrol.,2008

2. Crustal origin for peralkaline rhyolites from Kenya: evidence from U-series disequilibria and Th-isotopes;Black;J. Petrol.,1997

3. Ascent-driven crystallisation of dacite magmas at Mount St Helens, 1980–1986;Blundy;Contrib. Mineral. Petrol.,2001

4. Zircon saturation re-revisited;Boehnke;Chem. Geol.,2013

5. The Lu–Hf and Sm–Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets;Bouvier;Earth Planet. Sci. Lett.,2008

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