Taking the plate tectonics as leading theories, combining outcrop, seismic techniques, drilling and logging datum, inter-verifing manifold researching methods, The paper has amply researched the region. discussed the coupling relation of basin-mountain and the geodynamics system; analyzed geologic tectonic characteristics of the basin; confirmed superposed alteration in Mesozoic of the basin; recompartmentalized tectonic units of the researching region and the basin; studied the tectonic evolution of the basin since Mesozoic; ascertained four large tectonic layers and five tectonic evolution process stages in different ways of formation and tectonic alteration; established different tectonic stages黄色免费强奸视频网站、compages国产人看人碰人摸人澡、models and sedimentary filled processes, based on the organic geochemistry and oil-gas geologic characteristics in middle Cenozoic of the basin, the conclusions have been summarized in the paper, such as:The primary source rock in lower Permian and subordinate source rock in upper Triassic are developed in the region with better quality, and secondary hydrocarbon is possible; The bearing system which is comparted by three large tectonic layers and two unconformity surfaces formed in Palaeozoic中国区第一黄色网、upper Palaeozoic to Triassic and Cenozoic developing in the region, compounded with reservoirs of different lithology is developed in the region, while the property of tectonic fracture reservoir is better; Based on the analyzing petroleum accumulation elements and preserving conditions, the deep depressing belt in the north of Luoyang depressionwww.c黄、Shiling-Yiyang folded fault belt in Yiyang depression and wide anticline belt in Yichuan depression are advantageous petroliferous region, Zhaizhen anticline in Luoyang depression and Shimen wide anticline on footwall of overthrust in Yichuan depression are optimum tectonic traps.

本文以板塊構(gòu)造理論為指導(dǎo)思想，采用露頭區(qū)野外地質(zhì)與盆地地震国产迷晕暴力玩弄网站、鉆井午夜免费在线污视频一区二区三区、測(cè)井資料密切結(jié)合国产怡红院，多種測(cè)試方法互檢的研究方法，探討了盆山耦合關(guān)系及其所控制的地球動(dòng)力學(xué)系統(tǒng)成人免费在线观看网址视频；分析了研究區(qū)域和盆地地質(zhì)結(jié)構(gòu)構(gòu)造特征人人玩人人看人人靠,人人想人人操人人，確定了中生代盆地的疊合改造性質(zhì)，并重新劃分區(qū)域構(gòu)造單元和盆地構(gòu)造單元无码一级爽视频在线播放，深入研究了洛陽(yáng)—伊川盆地自中生代以來的構(gòu)造演化；確定了成盆作用和構(gòu)造改造作用的四大構(gòu)造層和五期不同方式中文字幕日本αv一区二区、方向的構(gòu)造演化過程AV线天堂久；建立了不同構(gòu)造階段的構(gòu)造組合和樣式及與構(gòu)造相關(guān)的沉積充填過程；在此基礎(chǔ)上通過多種有機(jī)地球化學(xué)指標(biāo)黑人粗进欧美白妞，研究盆地中新生代油氣地質(zhì)特征亚洲图片乱伦视频，認(rèn)為本區(qū)發(fā)育下二疊統(tǒng)區(qū)域主力烴源巖、上三疊統(tǒng)區(qū)域非主力烴源巖啪啪啪日韩，兩套烴源巖質(zhì)量均較好成年网站免费视频网站在线观看网址，并具備二次生烴條件；認(rèn)為本區(qū)發(fā)育古生界日韩手机在线视频久操、上古生界—三疊系和新生界三大構(gòu)造層在线播放A级毛片、兩個(gè)不整合界面分隔、不同巖性儲(chǔ)集層疊置組合和構(gòu)造裂隙型儲(chǔ)集層的復(fù)式儲(chǔ)集體系日本免费三网站，其中構(gòu)造裂隙型儲(chǔ)集層儲(chǔ)集性能較好国产一区二区久久精品；依據(jù)油氣成藏條件和保存條件分析，認(rèn)為洛陽(yáng)凹陷北部深凹帶人人操人人看人人拍、宜陽(yáng)凹陷內(nèi)石陵—宜陽(yáng)褶斷帶以及伊川凹陷伊川寬闊背斜帶為較有利含油氣區(qū)黄色网页在线欧美，有利的構(gòu)造圈閉是洛陽(yáng)凹陷翟鎮(zhèn)背斜和伊川凹陷的石門逆沖斷層下盤的寬緩背斜

Dawsonite of Mesozoic strata in Northeast China and adjacent area distribute in Lower Cretaceous strata from Hailaer basin,Tamtsag basin, Erlian basin, Kailu basin and Fuxin basin, and Upper part of Lower Cretaceous and Lower part of Upper Cretaceous from southern Songliao basin.

東北及鄰區(qū)中生代地層中的片鈉鋁石分布于海拉爾盆地、塔木察格盆地调教一区、二連盆地免费无码又爽又刺激A片涩涩、開魯盆地和阜新盆地的早白堊世地層及松遼盆地南部的早白堊世晚期-晚白堊世早期地層中。

Research of evolution of Poyang Lake Basin indicates that the basin changed from a intermontane basin into an inland accumulated basin in upper Pleistocene, and has become a loading and unloading basin adjusting water of Yangtze River since 400 A. D, which proves that influence of Yangtze River to Poyang Lake Basin appeared very late.

對(duì)鄱陽(yáng)湖盆地演化的分析發(fā)現(xiàn)啊使劲c我高清在线观看，該盆地于晚更新世開始從山間盆地向較大規(guī)模的積水盆地轉(zhuǎn)變超碰人妻久久，公元400年前后才成為調(diào)節(jié)，長(zhǎng)江水量的吞吐型湖盆影音先锋熟女AV下载电影，從而也反映出長(zhǎng)江對(duì)該區(qū)的影響是非常晚近的事一区二区精品在线。

Some of geological evolution process in Qinghai-Tibet plateau and were recorded in corresponding basins, By the research of sedimentary filling pattern and dynamic background at Cenozoic in Hoh Xii basin, Qaidam basin and Jiuquan basin, we can find that evolution sequences of these three basins are similar: strike-slip basin or extensional basin at the early stage. foreland basin at the middle stage, intermontane basin at the end.

對(duì)可可西里盆地、柴達(dá)木盆地和酒泉盆地新生代的沉積充填與盆地動(dòng)力學(xué)背景的研究發(fā)現(xiàn)精品国产三级在线天天更新，3個(gè)盆地的演化序列具有相似性日本免费第一网站，盆地的早期為走滑盆地或伸展盆地性質(zhì)，中期發(fā)育前陸盆地国模嫩模大尺度无码，最后以山間盆地結(jié)束干一干摸一摸。

To No. 20 are respectively black mudstone, black mudstone ( Caitun mining area of Benxi Basin,Paleozoic), dark grey gangue (Caitun mining area of Benxi Basin, Paleozoic), brown shale(Caitun mining area of Benxi Basin, Paleozoic), brown grey shale(The West Opencut Coal Mine of Fushun Basin, Cenozoic), grey silty mudstone(Haizhou Opencut Coal Mine of Fuxin Basin, Mesozoic), black grey gangue(Haizhou Opencut Coal Mine of Fuxin Basin, Mesozoic), grey yellow clay(Jianping County, Chaoyang City, its era to be determined), grey silicon slate( Qianshan Mountain of Anshan City, pre-Paleozoic), grey phyllite(Qianshan Mountain of Anshan City, pre-Paleozoic), granite-gneiss(Qianshan Mountain of Anshan City, pre-Paleozoic), granite(Mount Yiwulu, its era to be determined), diorite(Mount Yiwulu, its era to be determined), black basalt(The West Opencut Coal Mine of Fushun Basin, Cenozoic), dark purple andesite( Mount Guiyunhua of Zhuanghe City, Mesozoic), fragment of brick-tile-pottery-porcelain( from the building site of Panjin City), coal cinder( from the boiler room of Heji Road of Panjin City), cement( from the building site of Panjin City) and slag (from Bohai Stockroom of Liaohe Oilfield produced in Anshan City).

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Combined the geological analysis with analogue modeling experiments,the evolution of the Yinggehai basin could be divided into four main stages:(1) Before 42Ma,controlled by the southeastward extension of the Beibu Gulf basin on the northern continental margin,the Yinggehai basin experienced dextral pull-apart.Bounded by NS-trending Yingxi fault,the transtensional areas mainly are the northwest part and along the eastern boundary of the basin.(2) From 42 to 21Ma,the development of the main rift body in Yinggehai basin was mainly controlled by the southward slip and clockwise rotation of the Indochina block along the Red River fault zone,and the sedimentation was strengthened due to the sinistral transtension.In the east,the subsidence is deepened due to the dextral transtension.(3) From 21 to 10.4Ma,the sinistral movement of the Indochina block slowed down to still.From 21 to 15.5Ma,the northwest part of the basin began to inverse locally because of post-rift thermal subsidence of the whole basin.(4) From 10.4Ma to present,the basin was affected by the dextral movement of the South China block along the Red River fault zone and thermal accident in a new phase at 5Ma.

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Based on the petroleum system division of our predecessors, the petroleum systems of Chinese marine basin s can be divided into six types, that is, the aulacogen and its succeeding syneclise, the craton basin, the craton peripheral subsidence basin, the foreland basin, the strike slip basin and the epicontinental fault basin petroleum system.

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Luoyang-Yichuan basin is a multicycle superimposed continental sedimentary basin in middle Cenozoic, east of China. The basin has gone through such evolution stages as craton passive continental margin basin in Pre Mesozoic, depression basin in early Mesozoic, foredeep basin in late Mesozoic and fault depression basin in Cenozoic, etc. The Tectonic evolution of the basin is characterized by obvious multicycle superposition and multi-tectonism.

洛陽(yáng)—伊川盆地是中國(guó)東部中新生代疊合多旋回陸相沉積盆地，其形成主要經(jīng)歷了前中生代克拉通被動(dòng)大陸邊緣盆地日本黃色A片三級三級三級免费看、早中生代坳陷盆地黄色在线免费交配视频、晚中生代前淵盆地和新生代斷陷—坳陷盆地等演化階段，構(gòu)造演化具有明顯的多期次疊合黄色视频免费区，多構(gòu)造作用的特點(diǎn)久久一日本道色综合久久青草青草视频。

We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

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