| 昆中断裂东段不同时代蛇绿岩特征及形成环境 |
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| 引用本文： | 解玉月. 昆中断裂东段不同时代蛇绿岩特征及形成环境[J]. 青海国土经略, 1998, 0(1) |
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| 作者姓名： | 解玉月 |
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| 作者单位： | 青海省区调综合地质大队 |
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| 摘 要： | 沿昆中断裂带分布的两套不同类型的蛇绿混杂岩,均属非典型的蛇绿岩套残块(片),是昆中断裂带在漫长的地质演化过程中残留在陆块边缘的洋壳物质。它们在空间上分布于不同的构造部位,时间上分属于元古代和晚古生代。
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| 关 键 词： | 蛇绿混杂岩 昆中断裂带 |
FEATURES OF OPHIOLITE WITH DIFFERENT PERIOD IN THE EASTERN SECTOR OF MIDDLE KUNLUN FAULT AND ITS ORIGINAL ENVIRONMENT |
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| Xie Yuyue Regional Geologic Survey and Comprehensive Study Team of Qinghai Province. FEATURES OF OPHIOLITE WITH DIFFERENT PERIOD IN THE EASTERN SECTOR OF MIDDLE KUNLUN FAULT AND ITS ORIGINAL ENVIRONMENT[J]. QINGHAI GUOTU JINGLUE, 1998, 0(1) |
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| Authors: | Xie Yuyue Regional Geologic Survey and Comprehensive Study Team of Qinghai Province |
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| Affiliation: | Xie Yuyue Regional Geologic Survey and Comprehensive Study Team of Qinghai Province |
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| Abstract: | The two kinds of ophiolitic melange along the Middle Kunlun fault belong tothe residual block of non-typical ophiolite suite and are the residual oceanic crust on the con-tinental margin during the long geological evolution of the Middle Kunlun fault. Being Pro-terozoic and Late Paleozoic ophiolitic melange, they distribute in different structural posi-tion. |
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| Keywords: | ophiolitic melange Middle Kunlun fault belt |
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