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西藏白朗地区蛇绿岩火山岩中单斜辉石的化学特征
引用本文:李达周,王风阁,张旗,周云生.西藏白朗地区蛇绿岩火山岩中单斜辉石的化学特征[J].地质科学,1984,0(2):149-156.
作者姓名:李达周  王风阁  张旗  周云生
作者单位:1. 中国科学院地质研究所;2. 冶金部桂林地质研究所
摘    要:近年来,应用岩石的地球化学和矿物学特征区分不同构造位置的现代火山岩,已被人们所注意。同时,根据这种观测资料所确定的一般特征,亦已广泛地应用于古火山岩,并获得了一些古地质环境的概念。

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收稿时间:1981-09-02
修稿时间:1981-09-02;

CHEMICAL CHARACTERISTICS OF CLINOPYROXENES OF VOLCANIC ROCKS FROM THE OPHIOLITE AT BAINANG, TIBET
Li Dazhou,Wang Fengge,Zhang Qi,Zhou Yunsheng.CHEMICAL CHARACTERISTICS OF CLINOPYROXENES OF VOLCANIC ROCKS FROM THE OPHIOLITE AT BAINANG, TIBET[J].Chinese Journal of Geology,1984,0(2):149-156.
Authors:Li Dazhou  Wang Fengge  Zhang Qi  Zhou Yunsheng
Institution:1. Institute of Geology, Aoademia Sinica, Beijing;2. Geological Institute, Ministry of Metallurgy, Guilin
Abstract:Bainang ophiolitic complex is part of Yarlung Zangbo ophiolite zone. 14 clinopyroxen-es from pillow lavas and sheeted dike swarms in Bainang ophiolitic complex have been analysed. They are characterized by higher Mg, poorer Ti, Al and Fe and lower Ti/Al ratio in composition. They are similar to host rocks that have both features of mid-oceanic ridge and island arc basalts. Perhaps, it was a tectonic setting of island arc-margin basin. Wider range and complexity of compositions shown by both of basaltic rocks and the clinopyroxenes suggest that these rocks are probably derived from different magma sources.
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