| 造山带地层类型研究 |
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| 引用本文： | 王根宝,张月树.造山带地层类型研究[J].陕西地质,1999(2). |
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| 作者姓名： | 王根宝 张月树 |
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| 作者单位： | 陕西省地勘局西安地质矿产勘查开发院!长安710100 |
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| 摘 要： | 根据形成环境，造山带地层可分为三种类型：形成于稳定地台、地位、或大陆边缘，且后期无强烈构造置换的史密斯型，形成于板块或地体边缘，并经构造多期置换表现出构造（蛇绿）混杂岩特征的非史密斯型和与介于二者之间具构造岩片特征的过渡类型。
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| 关 键 词： | 地层类型 非史密斯型 过渡类型 造山带 |
STUDY OF STRATIGRAPHIC TYPES OF OROGENIC BELT |
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| Wang Genbao, Zhang Yueshu.STUDY OF STRATIGRAPHIC TYPES OF OROGENIC BELT[J].Geology of Shaanxi,1999(2). |
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| Authors: | Wang Genbao Zhang Yueshu |
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| Abstract: | Based on forming background, the strata of orogenic belt can be divided three types asfollows: (1) Speith type, formed in stable platform, terrane, or continental margin, whichdidn't take place any high tectonic replacement, (2) non-Smith type, formed in the marginof plate and terrane, went through more stages replacement, had the feature of tectonic(ophiolite) -mixtite, (3) tranitional type, between (1) and (2), had the features of tectonicfacies. |
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| Keywords: | stratigraphic type non-Smith type tranitional type orogenic belt |
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