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tectonic gneisses
相关语句
  构造片麻岩
     The ductile deformation belts in the basement of the central Tanlu fault zone in central Shandong can be divided into two types: (1) NE trending ductile deformation belts, which were formed before the emplacement of the Early and Middle Proterozoic granitic intrusives (2 488 Ma) and are characterized by the development of the middle and deep level tectonic gneisses;
     郯庐断裂中段鲁中基底的韧性变形带可分为两类:(1)北东向韧性变形带,以发育中深层次的构造片麻岩为特征,形成于早中元古代花岗质岩体(2488Ma)侵位之前;
短句来源
     The medium-high temperature ultra-ductile deformational rocks are composedof stratified granitic tectonic gneisses, foliated granitic tectonic gneisses and zonal granitic tectonic gneisses, which are related to orogeny in Jinning episode,detachments in early Caledoninnepisode and lndosinian episode, respectively.
     中高温超塑性变形岩石由层状花岗质构造片麻岩、面状花岗质构造片麻岩和带状花岗质构造片麻岩构成,它们分别形成干晋宁期造山作用、早加里东期和印支期的基底折离作用。
短句来源
     The gneiss series was formed by the tectonic gneisses of the Archean intrusive rocks through dynamic metamorphism and static recrystallization.
     该片麻岩系由太古宙侵入岩经动力变质作用、静态重结晶作用而形成的构造片麻岩类。
短句来源
  相似匹配句对
     Tectonic in Architecture
     论建筑中的结构造型
短句来源
     Criticize and Tectonic
     批判与建构
短句来源
     Petrochemistry and tectonic background of the gray gneisses in north Dabie terrane
     北大别灰色片麻岩的岩石化学特征及大地构造背景
短句来源
     Geochemistry, Geochronology and Tectonic Settings of Archean Gneisses in Lushan, Henan Province
     河南鲁山地区太古代片麻岩系的地球化学、锆石年代学及其构造环境
短句来源
     ORIGIN OF THE FUPING GNEISSES
     阜平片麻岩之成因
短句来源
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The deformation analysis of tectonic rocks in Wuchuan-Siliui faulting belts shows thatthere exist two series of tectonic rocks,i. e.,medium-high temperature ultra-ductile deformational rocks and semi-ductile and semi-brittle mylonites, which have a long and complex deformation history. The medium-high temperature ultra-ductile deformational rocks are composedof stratified granitic tectonic gneisses, foliated granitic tectonic gneisses and zonal granitic tectonic gneisses, which are related...

The deformation analysis of tectonic rocks in Wuchuan-Siliui faulting belts shows thatthere exist two series of tectonic rocks,i. e.,medium-high temperature ultra-ductile deformational rocks and semi-ductile and semi-brittle mylonites, which have a long and complex deformation history. The medium-high temperature ultra-ductile deformational rocks are composedof stratified granitic tectonic gneisses, foliated granitic tectonic gneisses and zonal granitic tectonic gneisses, which are related to orogeny in Jinning episode,detachments in early Caledoninnepisode and lndosinian episode, respectively. Semi-ductile and semi-brittle mylonites characterized by appearance of pseudotachylites are the products of thrust faulting in early Yanshanepisode.

吴川—四会断裂带存在着中—高温超塑性变形岩石和半韧性半限性糜使岩两大系列构造岩,具有长期复杂的变形历史。中高温超塑性变形岩石由层状花岗质构造片麻岩、面状花岗质构造片麻岩和带状花岗质构造片麻岩构成,它们分别形成干晋宁期造山作用、早加里东期和印支期的基底折离作用。而半韧性半脆性构造岩由糜棱岩系列岩石构成,尤以出现玻状岩为特征,为燕山早期逆冲断层产物。

The ductile deformation belts in the basement of the central Tanlu fault zone in central Shandong can be divided into two types: (1) NE trending ductile deformation belts, which were formed before the emplacement of the Early and Middle Proterozoic granitic intrusives (2 488 Ma) and are characterized by the development of the middle and deep level tectonic gneisses; and (2) NNE trending ductile deformation belts, which were formed in the Jinningian movement (941 Ma) accompanied by the development of...

The ductile deformation belts in the basement of the central Tanlu fault zone in central Shandong can be divided into two types: (1) NE trending ductile deformation belts, which were formed before the emplacement of the Early and Middle Proterozoic granitic intrusives (2 488 Ma) and are characterized by the development of the middle and deep level tectonic gneisses; and (2) NNE trending ductile deformation belts, which were formed in the Jinningian movement (941 Ma) accompanied by the development of middle and shallow level mylonites. A preliminary discussion is made on the formation mechanism and ages of the above mentioned two types of ductile deformation belts.

郯庐断裂中段鲁中基底的韧性变形带可分为两类:(1)北东向韧性变形带,以发育中深层次的构造片麻岩为特征,形成于早中元古代花岗质岩体(2488Ma)侵位之前;(2)北北东向韧性变形带,以中浅层次糜棱岩为特征,形成于晋宁期(941Ma)。文中对以上两类韧性变形带的形成机制和时代进行了初步讨论。

On the basis of the regional geological surveying(1∶50 000)in the Liuhe area, Jilin province,the Liushuhezi gneiss is studied in relatively detail.The gneiss is quite different from the common gneiss formed by euregional metamorphic deformation on geological features,e.g.rock size,structures and origin and so on.The gneiss series was formed by the tectonic gneisses of the Archean intrusive rocks through dynamic metamorphism and static recrystallization.The petrotectonics shows a diversity and a heterogeneity...

On the basis of the regional geological surveying(1∶50 000)in the Liuhe area, Jilin province,the Liushuhezi gneiss is studied in relatively detail.The gneiss is quite different from the common gneiss formed by euregional metamorphic deformation on geological features,e.g.rock size,structures and origin and so on.The gneiss series was formed by the tectonic gneisses of the Archean intrusive rocks through dynamic metamorphism and static recrystallization.The petrotectonics shows a diversity and a heterogeneity of the size structures,as well as a developed“blasto strain texture”.The rock texture and petrotectonics on space distribution exhibit a regular zonation.Aaccording to the unique texture of tectonic gneiss,a new term-“blasto strain texture”is proposed by the authers.Meanwhile,preliminary suggestion for the classification and nomenclature of tectonic gneiss is proposed.

在柳河地区开展1∶5万区调工作中,对测区内的柳树河子片麻岩做了较为详细的工作。结果认为,该片麻岩在地质特征、岩石粒度结构及成因等诸方面与传统认识上的纯区域变质作用所形成的片麻岩有较大的差异。该片麻岩系由太古宙侵入岩经动力变质作用、静态重结晶作用而形成的构造片麻岩类。其岩石构造具多样性、粒度结构具不均匀性,并具发育的变余应变结构。岩石结构和构造在空间分布上具有一定的分带性。笔者还根据构造片麻岩特有的结构提出了“变余应变结构”这一新的结构术语,并对构造片麻岩的分类命名提出了初步意见。

 
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