The foliations of mylonites in the two zones deeplydip to the north with nearly horizontal stretch lineation, dextral shear sense, and compressionaldeformation in the YZ face.

兩者均以糜棱面理往北陡傾、近水平的拉伸線理久久人妻系列无码专区、右行剪切應(yīng)變及在YZ面上的擠壓為基本特征无码肉片国产在线观看免费，為韌性&右行擠壓轉(zhuǎn)換型&剪切帶。

During early and middle Jurassic period, as a northern boundary, the fault zone controlled a seires of sedimentation of coal basins and magma activity. A lot of nappes developed during Ⅰ,Ⅱ and Ⅲ phase of the Yanshan movement. The strongest structural activity during the Yanshan movement is the Ⅱ phase, It had three pulsation and formed large-scale tectonic system with dextral strike slip.

早、中侏羅世国产人碰人摸人爱视频，斷裂帶作為北界狠狠亚洲婷婷综合色香五月加勒比，控制了由西向東一系列煤系盆地的沉積作用和巖漿活動亚洲综合偷拍一区二区三区；在燕山運動的Ⅰ欧美视频专区一二69久久、Ⅱ、Ⅲ幕中分別形成了一系列逆沖構(gòu)造欧美性交黄色视频；其中91交换，以燕山Ⅱ幕構(gòu)造活動最強，并至少經(jīng)歷了三次脈動作用久久毛片免费全部播放无码，形成的逆沖構(gòu)造不是由盆緣到盆內(nèi)的&對沖&久久久久国产精品片区无码，而是受本斷裂帶限制，并以之為主滑面構(gòu)成了區(qū)域上的大型右行走滑斜壓式構(gòu)造系統(tǒng)婷婷激情永久就去吻亚洲综合。

Here I reported new structural data to answer above question, including field section observations and geologic map with large scale in a key area, accompanying with detail microstructural observations, quartz C-axial fabric analyses, and tectono-thermogeochronology (40Ar/39Ar and zircon SHRIMP U-Pb method). Taking available previous data into account, following progression is achieved:1. Completely rebuilding the post late-Paleozoic deformation history of the Harlik MountainFive stages of deformation were identified:(1)pre-Permian compression deformation which may have resulted from pre-Permian subduction;(2) earlier Permian post-collision extension;(3) middle Permian west-east directed dextral slip shearing;(4) later Permian nearly N-S compression deformation; and (5) later Cenozoic intra-plate N-S compressional deformation.

本文選擇新疆東部哈爾里克山為研究對象激情综合欧美亚洲日韩，通過詳細(xì)的野外路線地質(zhì)構(gòu)造調(diào)查和關(guān)鍵地區(qū)大比例尺地質(zhì)填圖，以及室內(nèi)顯微結(jié)構(gòu)觀察性插视频在线播放、石英巖組分析和構(gòu)造熱年代學(xué)(Ar-Ar和鋯石SHRIMP U-Pb定年)研究国产特级毛片AAA多人毛，結(jié)合前人研究成果，取得了如下新進展：1精品久久久久久性色AV、系統(tǒng)重建了哈爾里克山晚古生代以來的變形歷史識別和確定了該區(qū)板塊俯沖碰撞階段的二疊紀(jì)以前擠壓變形久久伊人9，后碰撞階段早二疊世伸展變形、中二疊世近東西向右行走滑變形和晚二疊世近南北向擠壓變形影音先锋最新综合站资源，以及板內(nèi)演化階段的晚新生代南北向擠壓變形等5期構(gòu)造變形事件www.精选国产。

The effect of rod subsidence is the major error in each station. GPS velocity field in SW Taiwan indicates that the surface deformation reflect the movements of Chukou reverse fault, Hsinhua dextral fault, and detachment.

新化、觸口斷層一帶之GPS速度場分析成果顯示国产亚洲尤物臀足，此地區(qū)之地表位移量反映觸口斷層向西逆沖激情小说亚洲图片，新化斷層淺部鎖住、深部為右移之側(cè)向滑動aaa精品视频在线观看免费，及基底滑脫面向西逆沖三者作用累加的結(jié)果性欧美激情在线观看。