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
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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:
地质学报(英文版)
影响因子:
--
通讯作者:
XIANG Zhongjin, YAN Quanren, YAN Zhen, WANG Zongqi
XIANG Zhongjin, YAN Quanren, YAN Zhen, WANG Zongqi
中科院分区:
其他
文献类型:
--
作者:
XIANG Zhongjin, YAN Quanren, YAN Zhen, WANG Zongqi

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陶河口组是大巴山北方早志留世的一套火山沉积岩系。火山岩以碱性玄武岩为主,少量地幔捕虏体,富含单斜辉石斑晶。地球化学
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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