首页> 外文期刊>Science in China. Series D, Earth sciences >Geochemistry of the ophiolite and oceanic island basalt in the Kangxian-Pipasi-Nanping tectonic melange zone, South Qinling and their tectonic significance
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Geochemistry of the ophiolite and oceanic island basalt in the Kangxian-Pipasi-Nanping tectonic melange zone, South Qinling and their tectonic significance

机译:南秦岭康县-皮帕斯-南平构造混杂带蛇绿岩和海洋岛玄武岩的地球化学特征及其构造意义

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摘要

Detailed studies indicate that Kangxian-Pipasi-Nanping tectonic zone is a complicated melange zone which includes many tectonic slabs of different origins. Ophiolite (MORB-type basalt), oceanic island tholeiite and alkaline basalt have been identified. Moreover, this tectonic melange zone is eastward connected with the Mianluee suture zone. The deformation characteristics, consisting components and volcanic rock geochemical features for the Kangxian-Pipasi-Nanping tectonic melange zone are much similar to those of the Mianluee suture zone and Deerni ophiolite. Therefore, the Kangxian-Pipasi-Nanping tectonic melange zone should be the westward extension part of the Mianluee suture zone. It indicates that the Mianlue suture zone had extended to the Nanping area.
机译:详细的研究表明,康县—皮帕斯—南坪构造带是一个复杂的混杂带,其中包括许多不同起源的构造板块。已鉴定出蛇绿岩(MORB型玄武岩),大洋岛菱铁矿和碱性玄武岩。此外,该构造混杂带向东与Mianluee缝合带相连。康县—皮帕斯—南坪构造混杂岩带的变形特征,组成成分和火山岩地球化学特征与绵露缝合带和迪尔尼蛇绿岩的变形特征非常相似。因此,康县—皮帕斯—南平构造混杂带应为绵略缝合带向西延伸。说明绵略缝线带已延伸至南平地区。

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