The tectonic evolution of southern Junggar basin can be classified into seven stages: stage of intracontinental rift from middle Periman to late Late Carboniferous; stage of weak extension and peneplane from late Permian to early Triassic; stable depression stage in middle-late Triassic; maximal basin formation phase in the setting of weak extension in early-middle Jurassic; inactive depressed basin formation phase in thrust setting in middle-late Jurassic; stable depression stage in Cretaceous and Eogene; foreland depressed basin formation phase in thrust setting in Neocene and Quaternary.

準(zhǔn)噶爾盆地南緣晚石炭世以來盆地構(gòu)造演化可劃分為七個(gè)演化階段：晚石炭世—中二疊世陸內(nèi)裂谷作用階段国内一级黄色a片；晚二疊世到早三疊世處于弱伸展-穩(wěn)定坳陷作用階段人人操人人人；中欧美一级婬片A片免费播放口、晚三疊世準(zhǔn)平原化作用階段日日摸夜夜摸人人看亚洲综合；早午夜粉嫩粉嫩、中侏羅世為弱伸展背景下廣盆形成階段国产在线观看入口；中、晚侏羅世沖斷背景下的坳陷盆地形成階段亚洲一区精品劲爆儿视频；白堊紀(jì)到古近紀(jì)弱伸展背景下的穩(wěn)定坳陷盆地形成階段一东京热AAAAA片AAA一；新近紀(jì)—第四紀(jì)為沖斷背景下的前陸坳陷盆地形成階段。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

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The evolution process under the control of the multigeodynamic force system (including the boundary forces of Eurasia-Pacific-Indian three massive plates around Nansha block, effects of the deep mantle, relative soft layer-sliding planes within Nansha lithosphere block and the earth's rotational inertial force) can be briefly divided four stages: the late Cretaceous to the early Eocene stage of uprilfing-erosion and shear-extension caused by the oceanwards-eastwards withdrew of Pacific subduction zone and the delamination of proto-subducted slab after the stage of pre-Cretaceous pre-rifting active continentoceanic plate margin. In this stage, the Nansha transcrustal layering-block started to move southeastwards on the Nansha transcrustal layer-sliding plane, meanwhile, the Andu-Bisheng and Liyue-Banyue basement layering-block slid on their upper-crust layer-sliding planes, and Xibu accretion zone was formed. Successively, it entered the stage of the mid-Eocene to early Oligocene, when NW-SE sea-floor spreading occurred in the southwest subbasin owing to the slip-line field initiated by the collision between the Indian and Eurasian plates, Zengmu foreland-basin started to develop in the same time. And in the stage of late Oligocene to early Miocene, near NS simple-shear extension and sea-floor spreading in the central subbasin of eastern South China Sea resulted from the south-southeastwards drawing-force of the mantle-flow. The crustal layering-blocks and the Miri accretion zone formed also in this stage.

南沙巖石圈新生代微板塊及板內(nèi)層塊構(gòu)造的動(dòng)力演化過程一级免费ww视频，在多元?jiǎng)恿Φ纫蛩?如塊體之外的歐-太-印三大板塊運(yùn)動(dòng)邊界力和地幔深部活動(dòng)因素花蝴蝶免费视频高清版下载、塊體內(nèi)部軟弱層滑面以及地球自轉(zhuǎn)變化)控制下，大致經(jīng)歷了4個(gè)階段的演化：從前晚白堊世的裂前活動(dòng)陸-洋板塊邊緣階段因太平洋俯沖帶向東躍遷青草线观看免费观看视频、原向NNW俯沖消亡的板片的拆沉美国一级A片AAA欧美、幔隆而進(jìn)入晚白堊世-早始新世的隆升剝蝕、剪切伸展演化階段，南沙超殼層塊順超殼層滑面祥東南運(yùn)移在线观看午夜国产猫咪影院视频免费、安渡-畢生與禮樂-半月基底層塊沿上殼層滑面拆離欧美日韩有码A，西布增生帶形成；繼而先后在中始新世-早漸新世期間受印-歐板塊碰撞滑線場日韩中文激情无码迅雷下载视频、地球自轉(zhuǎn)加速影響出現(xiàn)西南海盆NW-SE向海底擴(kuò)張和曾母前陸盆地的發(fā)育，和晚漸新世-早中新世期間南—東南向地幔流牽引造成的中央次海盆近NS向單剪伸展與海底擴(kuò)張亚洲国产日韩欧美、殼體層塊向南差異滑移在线播放欧美9797影院、米里增生帶形成；中中新世以來中文字幕一级毛片在线，印度-澳洲板塊快速向北俯沖国产真实乱子精品视频，構(gòu)成今日南海格局。

The geotectonic evolution in east Tarim b asin has involved seven stages:basement formation in the pre-Sinian,faulted blocking of continental margin in pre-Caledoni an epoch,sag stage in late-Caledoni an epoch,foreland upwarp from Hercyni an to Indo-Chinese epoch,foreland b asin from Indo-Chinese to pre-Ye nshan epoch,intracontinental sag b asin in late-Yenshan epoch and faulted b asin in Himalayan epoch.

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根據(jù)Ar-Ar熱年代學(xué)研究，精確測定了早二疊世伸展變形和晚二疊世擠壓變形的峰期時(shí)代分別為290Ma和259Ma.2国产精品igao视频网网址免费播放、提出了關(guān)于哈爾里克山南麓小鋪一帶變質(zhì)帶和變質(zhì)作用的新認(rèn)識(shí)根據(jù)顯微觀察資料和特征變質(zhì)礦物的出現(xiàn)欧美熟妇另类，把小鋪一帶的變質(zhì)巖由SW向NE方向依次劃分為黑云母帶、石榴石帶人人摸人人爽一及片、十字石帶91色视在线网站免费观看、紅柱石帶和矽線石帶等變質(zhì)帶；初步確定該區(qū)的變質(zhì)作用屬于中溫-低壓型无码一区二区三区av免费，變質(zhì)作用發(fā)生的時(shí)代為290Ma左右夜夜摸天天做天天爽免费视频，是該區(qū)早二疊世地殼伸展的產(chǎn)物。3黄片你懂的、首次提出哈爾里克山南麓在石炭紀(jì)可能發(fā)育弧后盆地的新觀點(diǎn)根據(jù)哈爾里克山南麓原&居里得能組&巖屑砂巖的碎屑鋯石SHRIMP U-Pb定年视频在线黄色一区，確認(rèn)這套地層的沉積不早于晚泥盆世，很可能是石炭紀(jì)aaaaaa性欧洲，而不是前人所說的前寒武紀(jì)日本黄色视频在线免费；結(jié)合對(duì)其區(qū)域地質(zhì)背景、源區(qū)位置和沉積環(huán)境分析国产天天在线视频，推測該區(qū)石炭紀(jì)可能為滯后弧后盆地和弧后隆起區(qū)構(gòu)造背景激情小说激情图片激情视频。4、進(jìn)一步證明哈爾里克山不發(fā)育與島弧演化相關(guān)的泥盆紀(jì)巖漿活動(dòng)根據(jù)對(duì)代表性閃長巖和花崗巖的鋯石SHRIMP年代學(xué)研究獲得的新資料成性交免费视频，結(jié)合該區(qū)已有相關(guān)資料的綜合研究人人干人伦人人干，確定哈爾里克山巖漿巖分別形成于奧陶紀(jì)-志留紀(jì)和石炭紀(jì)晚期-二疊紀(jì)，不存在泥盆紀(jì)的巖漿巖，進(jìn)而認(rèn)為該區(qū)泥盆紀(jì)不屬于島弧環(huán)境性爱视频毛片。5在线播放免费黄色网页视频、重建了哈爾里克山古生代以來的地質(zhì)演化過程根據(jù)區(qū)域資料以及本次研究所獲得的資料，把哈爾里克山古生代以來的構(gòu)造演化劃分中奧陶世-早志留世為島弧www.yes235.com、中志留世-晚泥盆世為弧后區(qū)2区在线免费观看视频、石炭紀(jì)弧后伸展、二疊紀(jì)為后碰撞伸展與擠壓日韩精品老熟女系列视频在线、中生代差異隆升和晚新生代陸內(nèi)再造山過程等構(gòu)造階段18禁止看网站。6、初步估算了哈爾里克山地殼縮短率和縮短量根據(jù)前中生代地層褶皺估算的哈爾里克山南山口-口門子老女人肏屄视频、石城子-白石頭和沁城-小鋪三條剖面的地殼縮短率分別為16.2%免费超碰在线观看、19.8%和20.1%，相應(yīng)的地殼縮短量分別為4.3km美女让男人扒开退桶出白浆、9km和11.3km国产一级A∨国产片免费。

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