| 西太平洋板内造山作用模式中的大地构造相 |
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| 引用本文： | 许靖华. 西太平洋板内造山作用模式中的大地构造相[J]. 中国石油大学学报(自然科学版), 1994, 0(5) |
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| 作者姓名： | 许靖华 |
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| 作者单位： | Geological Institute，ETH Zentrum，CH- 8092 Zurich，Switzerland |
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| 摘 要： | 山脉的演化可与植物的生长过程作类比以西太平洋地质为例，对大地构造相进行了系统论述。在任何单一或组合的弧－弧、弧－陆及陆－陆碰撞过程中所形成的具有特殊构造式样的大地构造单元称为大地构造相。大地构造相有三个基本相型：日尔曼相以沉积盖层的薄皮构造变形为特征，凯尔特相以区域变质和剪切变形为特征，瑞替相以刚佐基底的逆掩构造为特征。本文采用大地构造柏分析方法对中国地质和阿尔卑斯山的成因提出了新的认识。
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| 关 键 词： | 大地构造相；日尔曼相；凯尔特相；瑞替相；西太平洋地质 |
TECTONIC FACIES IN A WEST PACIFIC MODEL OF INTRA-PLATE OROGENESIS |
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| Xu Jinghua. TECTONIC FACIES IN A WEST PACIFIC MODEL OF INTRA-PLATE OROGENESIS[J]. Journal of China University of Petroleum (Edition of Natural Sciences), 1994, 0(5) |
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| Authors: | Xu Jinghua |
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| Abstract: | The evolution of mountains is a process comparable to the growth of a plant.The con- cept of tectonic facies is demonstrated with West Pacific geology. The tectonic facies is designation ofthe unique tectonic style and is used to describe tectonic units that are formed by any combination ofarc-arc,arc-continent,or continent-continent collisions.There are three fundamental tectonic fa-cies,including Alemanide to describe the tectonic facies of thin-skinned deformation of sedimentarycover,Celtide to designate those facies that are characterized by metamorphism and/or shearing defor-mation,and Rhaetide to designate the structures dominated by rigid-basement overthrusting.The geol-ogy of China and the origin of the Alps are reinterpreted with tectonic facies analysis. |
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| Keywords: | Tectonic facies Alemanide Celtide Rhaetide West Pacific geology |
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