Equilibrium between Clinopyroxene and Host Rocks: Implication for the Magmatic Source and Evolution of Alkali Basalts of the Taohekou Formation in the Northern Daba Mountains, China
Equilibrium between Clinopyroxene and Host Rocks: Implication for the Magmatic Source and Evolution of Alkali Basalts of the Taohekou Formation in the Northern Daba Mountains, China
复制标题
单斜辉石与围岩的平衡:对大巴山北部桃河口组碱性玄武岩岩浆来源及演化的启示
DOI:
10.1111/j.1755-6724.2011.00386.x
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发表时间:
2011-02
期刊:
影响因子:
--
通讯作者:
XIANG Zhongjin, YAN Quanren, YAN Zhen, WANG Zongqi
中科院分区:
文献类型:
--
作者:
XIANG Zhongjin, YAN Quanren, YAN Zhen, WANG Zongqi
The Taohekou Formation is a volcanic‐sedimentary terrane formed in the early Silurian in the northern Daba Mountains, China. The volcanic rocks, with dominant alkali basalts and minor mantle xenoliths, are enriched in clinopyroxene phenocrysts. Geochemica
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影响因子:
3.5
作者:
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Acta Geologica Sinica ‐ English Edition
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