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滇西北点苍山蛇绿混杂岩的发现及意义
Discovery and significance of ophiolitic melanges at Diancang Mountain in northwestern Yunnan
【摘要】 点苍山西坡李子坪村分布有较多橄榄岩,围岩是一套中浅变质岩系,其中有斜长角闪岩、变质钠长花岗岩。这些岩石的岩相学、岩石化学及地球化学均显示蛇绿混杂岩特征,暗示点苍山西坡有古特提斯洋壳的残片存在。
【Abstract】 A lot of peridotites are distributed at Liziping Village on the western slope of Diancang Moun-tain.Their country rocks are a medium-and low-grade metamorphic series,consisting of amphibolite and metamorphosed albite granite.The petrography,petrochemistry and geochemistry of these rocks all indicate the features of ophiolitic melanges,suggesting the existence of relict fragments of the Paleo-Tethys oceanic crust on the western slope of Diancang Mountain.
- 【文献出处】 中国地质 ,Chinese Geology , 编辑部邮箱 ,2002年01期
- 【分类号】P588.3
- 【被引频次】11
- 【下载频次】146