The Garzê-Litang fault belt has experienced a series of complex evolutionary processes since the Paleozoic and is a large-scale, structurally complex ophiolitic mélange belt that has been strongly reworked and dismembered by overthrusting and sinistral strike-slip shear during the Cenozoic Himalayan orogeny.

提要： 甘孜—理塘斷裂帶自古生代以來經(jīng)歷了一系列復(fù)雜的演化過程人人干,人人拍,人人吊,人人操，為一規(guī)模宏大羞羞漫画www、結(jié)構(gòu)復(fù)雜并受到新生代喜馬拉雅期逆沖推覆和左行平移走滑剪切作用強(qiáng)烈改造肢解的蛇綠混雜巖帶韩国2022最新理论电影。

Our results indicate that the basin is comprised of three depressions with some sedimentary centers and is characterized by sinistral echelon during the Palaeogene.

研究結(jié)果表明嗯啊一区视频在线观看，柴北緣盆地在古近紀(jì)由三條北西向凹陷帶組成人妻在线交插，具有多個沉積中心欧美黄色小视频在线，平面上呈現(xiàn)左行雁列；在新近紀(jì)總體上呈北西-南東向?qū)挷蹱钫共?5免费视频，附有局部小型凹陷?/p>

Tan-Lu fault zone ; sinistral strike-slip ; 40 Ar/39 Ar plateau age ; Rb-Sr isochron age

郯廬斷裂帶国产春色一级视频免费；左行走滑斷裂；（40）~Ar/（39）~Ar坪年齡激情小说另类； Rb-Sr等時(shí)線年齡

SIR C/X SAR ; The Kuqa thrust belt ; Sinistral strike slip ; Flower structures ; Fractal dimension

航天飛機(jī)SIR-C/X-SAR 中文在线中文字幕；庫車沖斷帶；左行走滑操美女6666；花狀構(gòu)造人日人视屏；分?jǐn)?shù)維

They are:①completed total 8 000 km long natural seismic profiles cross the northern boundary and central part of the plateau, identified several deep-cut lithospheric faults and low velocity and low density bodies under the central part of the plateau related to Cenozoic volcanic eruption, the Tarim block subducted beneath the Altun Mts;②found the evidence that the Altyn Tagh fault formed in 220～240 Ma and at least 400 km sinistral offset since, and determined quantitatively deformation in Cenozoic;③discovered 350 km long high-ultrahigh pressure metamorphic belt in the south border of the Qilian terrane,which brobably represented the Early Paleozoic boundary between the North China and Yangtze plates;④according to new discoveries of caledonian ophiolite,granite are subducted complex established paleo-collision orogenic framework of northern Qinghai-Tibet plateau;⑤proposed a new model .

本文展示了中法1995～2000年青藏高原北部地學(xué)研究的如下主要新進(jìn)展：①完成8 000 km長的青藏高原北部及中部天然地震巖石圈探測剖面，確定若干條巖石圈斷裂毛片免费看不卡网站，發(fā)現(xiàn)與新生代火山噴發(fā)有關(guān)的青藏高原中部深處的低速亚洲国产一区区三区在线播放、低密度體，塔里木地塊俯沖于阿爾金山之下美女黄色视；②提出阿爾金斷裂形成于220～240 Ma和左行平移400 km的科學(xué)依據(jù)及確定其新生代變形量国内视频偷拍网站；③確定祁連南緣350 km長的高壓-超高壓變質(zhì)帶，提出其可能代表早古生代時(shí)期北中國板塊與揚(yáng)子板塊之間西部界限的新認(rèn)識亚洲综合激情另类小说；④根據(jù)加里東期蛇綠巖国产欧美视频一区二区色老头影视、花崗巖及俯沖雜巖帶的新發(fā)現(xiàn)美女顶级依人在线视频观看，初步建立了古碰撞造山格架；⑤提出高原隆升的&地幔底辟和內(nèi)向陸內(nèi)俯沖&的新假設(shè)97爱爱。

The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle.

中生代左行走滑和早第三紀(jì)伸展作用共同控制了渤海海域早第三紀(jì)的構(gòu)造格局93一区=区三区持级黄色毛片。

A series of dongas and valleys cut by the rupture show isochronous sinistral strike slip, the slip rate is 13.4～16.8mm/a on an average that belongs to AA activity level.

流經(jīng)破裂帶的一系列溝谷發(fā)生左旋同步扭曲，平均滑動速率為13 4～16 8mm a欧美高清不卡A片快爽，屬AA級活動水平国产强伦姧在线观看。

K-Ar whole-rock analysis of mylonites from a sinistral strike-slip ductile shear zone in the southern part of the Tan-Lu fault zone suggests that after its formation the shear zone cooled to the closure temperature 99±2 Ma ago Cat the end of the Early Cretaceous.

對郯廬斷裂帶南段左旋走滑韌性剪切帶中糜棱巖的K-Ar全巖分析結(jié)果研究表明，該剪切帶形成后一级电影三级电影，在99±2 Ma前冷卻至封閉溫度www.av.。

The internal deformation indicates that the pluton experienced sinistral spiral ascent and final ballooning emplacement.

內(nèi)部構(gòu)造變形特征表明鳳凰山巖體在深部主要為左旋螺旋式強(qiáng)力上升，淺部為氣球膨脹式主動侵位www.日韩.com。

This sinistral faulting resulted from high-speed NNW-oblique subduction of the Izanagi plate in the Pacific region, and represents the typical Peri-Pacific tectonic regime and the turning point of the tectonic framework in East China.

這次左行平移是太平洋區(qū)伊澤納崎板塊向北北西向高速斜向俯沖的結(jié)果国产欧美高清，屬于典型的濱太平洋構(gòu)造，可能代表了中國東部構(gòu)造格局轉(zhuǎn)換的開始在线观看你懂的网站免费不卡。