Origin of high-An plagioclase in the early Permian (~280 Ma) Xiaohaizi wehrlite, Northwest China: insights from melt inclusions in clinopyroxene macrocrysts and zircon oxygen isotopes
Origin of high-An plagioclase in the early Permian (~280 Ma) Xiaohaizi wehrlite, Northwest China: insights from melt inclusions in clinopyroxene macrocrysts and zircon oxygen isotopes
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中国西北早二叠世(~280 Ma)小海子韦尔岩中高安斜长石的成因:来自单斜辉石巨晶和锆石氧同位素中熔体包裹体的见解
DOI:
10.1080/00206814.2015.1136799
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发表时间:
2016-01
影响因子:
2.6
通讯作者:
Zhen-Yu Luo
中科院分区:
文献类型:
--
作者:
Xun Wei;Yi-Gang Xu;Zhong-Yuan Ren;Zhen-Yu Luo
ABSTRACT The Xiaohaizi wehrlite intrusion in the early Permian Tarim Large Igneous Province, Northwest China, is characterized by unusual high-An (up to 86) plagioclases. It has been suggested that H2O may have exerted a major control on their formation,
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