metamorphic core complex
- 网络变质核杂岩
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The metamorphic core complex is an important rheologic pattern of continental extension .
变质核杂岩是大陆流变伸展的重要表现形式。
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The Xiaoqinling metamorphic core complex experienced two stages of extension with different mechanism .
作为中国金矿主产地之一,小秦岭变质核杂岩经历两期不同性质的伸展。
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Metamorphic core complex structure with rich characteristics ;
四是庐山山体是一个典型而富有特色的变质核杂岩构造;
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Characteristics of Fangshan metamorphic core complex , beijing and a discussion about its origin
北京房山变质核杂岩的基本特征及其成因探讨
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The high sr , low y granite in the metamorphic core complex and its geological significance
变质核杂岩中高Sr低Y型花岗岩的发现及其地质意义
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Really exist postorogenic metamorphic core complex in Western henan ?
豫西后造山阶段存在变质核杂岩吗?
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Determination of metamorphic core complex in East Pamir
东帕米尔变质核杂岩构造的厘定
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Extensional kinematics and shear type of the Hohhot metamorphic core complex , Inner Mongolia
呼和浩特变质核杂岩伸展运动学特征及剪切作用类型
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The study of the metamorphic core complex has important significance for the understanding of the crustal evolution and mineral exploration in southeastern Yunnan .
对该变质核杂岩的研究,将对滇东南地区的地壳演化认识及矿田勘查有重要意义。
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It is therefore held that the Yiwulushan metamorphic core complex system must have played an important controlling role in the formation of gold deposits .
医巫闾山变质核杂岩构造系统对区内金矿有一定控制作用。
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A preliminary study indicates that genetically , the deposit is related to the Qungdo'gyang metamorphic core complex , longitudinal faults and Jurassic stratum .
初步分析矿床与北部的穷多江变质核杂岩、广泛发育的南北向断裂及侏罗纪地层有着密切成因联系。
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The results of this research list below : ( 1 ) Liaonan metamorphic core complex has a three-layer structure and is constituted by five parts .
获得以下成果:(1)对辽南变质核杂岩的主拆离断层带及其构造-岩浆关系开展了深入研究。辽南变质核杂岩具有三层结构,由五部分组成。
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The composition and texture of the metamorphic core complex show features of symmetrical extension and asymmetric uplifting and a rapid uplifting period within 130 to 100 Ma .
变质核杂岩的组成与结构显示了它对称伸展和不对称隆升的特征,130~100Ma是其快速隆升的时期。
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Yiwul ü shan mountain is proved to be a metamorphic core complex formed in Cretaceous according to field survey , microstructural analysis , and isotropic dating .
经过野外宏观观测、室内显微分析及同位素年龄测定,基本厘定医巫闾山是一个白垩纪时形成的变质核杂岩。
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The metamorphic core complex of South Kalatag is located in the Zhongtianshan terrane in the Dongtianshan region .
喀拉塔格南变质核杂岩位于东天山地区中天山古陆中,为大陆边缘型变质核杂岩构造。
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Deformation Characteristics of Middle Ductile Rheological Bed of the Yiwul ü shan Metamorphic Core Complex in Western Liaoning Province Journal of Shanxi Medical University ( Preclinical Medical Education Edition )
辽西医巫闾山变质核杂岩中间流变层变形特征山西医科大学学报(基础医学教育版)
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The evolution of the XMSZ demonstrates that the North Dabie dome is a metamorphic core complex developed in the Dabie orogenic belt during post-orogenic extension .
晓天-磨子潭剪切带的演化指示北大别穹隆是大别造山带晚造山伸展过程中形成的变质核杂岩。
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Meanwhile , its emplacement is closely related to the Liaonan metamorphic core complex , so this point provides an uncommon opportunity to studying the tectonic mechanism of the early Cretaceous magmatism .
同时,该花岗岩的侵位与辽南变质核杂岩密切相关,这为我们研究早白垩世岩浆活动的构造体制提供了难得的机会。
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According to a detailed study of Early Proterozoic extensional structures on the eastern margin of Northern China Platform and comparison with the metamorphic core complex , an uplift-bedding slide structural model has been put forward .
研究华北地台东部边缘早元古代拉伸构造及与变质核杂岩的比较,提出了隆-滑构造模式。
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The south and north sides of the metamorphic core complex are all grown in the large scale superposed basin , and north side forms a " young " straight fault and syntectonic magmatic rock .
核杂岩南、北侧发育上叠盆地,北侧形成年轻正断层及同构造期岩浆岩。
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In the metamorphic core complex ( MCC ) and the metamorphic arch , Jiangxi and Hunan area , there is an obvious correlation between the late brittle fault and the early subordinate ductile structure .
赣湘地区的变质核杂岩和变质穹窿构造中,晚期脆性断裂与早期低序次韧性构造间存在着明显的相关联系。
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In light of long run thermal evolution of the concerned area , the Harkin metamorphic core complex can be considered as a typical example of crust extension caused by thermal upwelling of mantle and intrusion of magma .
从该区长期的热演化历史以及同构造的岩浆活动来看,可以认为喀喇沁变质核杂岩是地幔热隆及岩浆侵入引起地壳伸展的典型实例。
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The metamorphic core - complex structre in South Liaoning
辽南变质核杂岩构造
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The study of geological action of fluid inclusions is important for us to know the condition of formation , the tectonic evolution and the dynamics process about high-pressure , ultrahigh-pressure metamorphic and core complex .
流体的地质作用研究对于了解高压、超高压变质岩及变质核杂岩的形成条件、构造演化和动力学过程具有重要意义。