昆中蛇绿岩岩石学和地球化学  

The Petrology and Geochemistry of ophiolites from Central Kunlun

作　　者：李丽[1] 董福辰[1] 杨永强[2] 朱志新 姜寒冰[1] 辛江[2] 

机构地区：[1]西安地质矿产研究所,陕西西安710054 [2]中国地质大学地质过程与矿产资源重点实验室,北京100083 [3]新疆维吾尔自治区地质调查院,新疆乌鲁木齐830000

出　　处：《新疆地质》2012年第1期19-25,共7页Xinjiang Geology

摘　　要：作为昆南变质地体与柴达木-中阿尔金地块边界的中昆仑缝合带,沿带断续出露蛇绿杂岩.本次研究涉及布青山蛇绿岩、诺木洪蛇绿岩和阿其克库勒湖西缘蛇绿岩,通过对其岩石学、岩石化学和微量元素与稀土元素地球化学特征分析,确定其属蛇绿岩类,证明蛇绿杂岩带性质属板块缝合带.The intermittent ophiolites may be regarded as important petrological criterias for recognition of suture zone in central Kunlun, which is the boundary of metamorphic terrane in southern Kunlun and block in Qaidam and central Altun. The petrology, petrochemistry, REE and trace elements of ophiolites, such as Buqingshan, Nuomuhong and Aqikekulehu, indicate that they belong to ophiolites and the ophiolite belt may be the suture zone.

关 键 词：中昆仑 岩石学 地球化学 蛇绿岩 缝合带 

分 类 号：P584[天文地球—岩石学]