In literature[1] Thrust Belt Structure and Significance for Petroleum Exploration in Hala'alat Mountain in Northwestern Margin of Junggar Basin, the Triassic and Permian strata in Heshituologai basin, which were used for supporting its proposed tectonic pattern s, are in big differences compared with the actual geologic data.

在《準噶爾盆地哈拉阿拉特山?jīng)_斷帶構造及找油意義》一文中性色网站污视频，用于支持其構造模式成立的和什托洛蓋盆地的三疊系和二疊系具有很大的推測成分超碰a，與實際地質(zhì)資料差別大。

Then through building modes of Mountain Hala'alat and faults controlling basin, it is thought that uplifting of mountain, subsidence of Wuxia fault belt and Heshentologa innertief basin have close relation to circle of landmasses, strike slip motion of marginal faults, so"Transpression Model"and"Differential Circling, Departure Up And Down Model"are proposed.

通過建立哈山及控山控盆斷裂的構造模式欧洲精品乱码久久久久，認為哈山的隆升欧美一区欧美一区、烏夏斷裂帶的沉降及和什托洛蓋盆地的發(fā)育與地塊間的相互旋轉(zhuǎn)、盆地周緣走滑斷裂的旋向關系密切毛片点击进入免费看，因此符合壓扭構造模式和&差速旋轉(zhuǎn)A级毛片视频、上下脫耦&模式。

Jianghan Basin is a representative inland salt-lake fault basin with an unique structural evolution history and petroleum geologic conditions. More than forty years of exploration activities have found over a hundred millions of proved reserves in place, and nearly two thirds of hydrocarbon resources to be proved. With the increasingly maturative exploration, the exploration direction research should be done as soon as possible.

江漢盆地是我國東部一個典型的內(nèi)陸鹽湖斷陷盆地十大免费涩视频，具有十分獨特的構造演化歷史和成藏地質(zhì)條件日本熟女强奸乱码，經(jīng)過四十余年勘探已經(jīng)發(fā)現(xiàn)一億多噸探明石油地質(zhì)儲量，還有近三分之二的油氣資源待探明久久精品中文字幕av，隨著勘探程度提高99热这里只有精品久久，勘探方向亟待深入研究。

The results show that the multi-stage and multicycle of tectonic movement in China continent result in the superimposed basin pattern which has many types of basin and mountain coupling systems with multi-stages.

結(jié)果表明视频在线精品，由于中國大陸構造運動的多期次和多旋回性形成的疊合盆地格局九色自拍视频在线观看，不但發(fā)育有多種類型的盆山耦合關系，而且造成盆山耦合的多階段性黄的视频黄的网站。。

The multicycle tectonic evolution of Tarim craton controls the formation of superimposed the Tarim Basin,petroleum-geology conditions as well as the features of composite petroleum system ,thus determines hydrocarbon distribution and resources potential in the basin.

塔里木克拉通多旋回構造演化控制了塔里木疊合盆地的形成及石油地質(zhì)條件和復合含油氣系統(tǒng)特征www日韩网站，進而決定了油氣的分布和資源潛力。

Ordos Basin is a large multicycle superimposed basin, developed on the basement of early Proterozoic crystalline basement.

疊合盆地由于其形成演化国产十八禁黄无遮禁视频免费、沉積建造的多旋回性国产美女特级片免费视频播放器，因而油氣勘探具有勘探難度大、勘探時間長好大好深好猛好爽好湿视频、勘探潛力大的特點国产v亚洲v日韩v欧美v天堂Ⅴ。

Based on the date of outcrop, log and lithology, sequence stratigraphic division and correlation were made on Neopaleozoic in south of North China Basin, and high-precision geologic correlation framework was built up in the basin.

以露頭、測井和巖性資料為基礎老熟精品视频在线观看，對華北盆地南部上古生界進行了層序地層的劃分與對比工作山外精品影院，建立了盆地范圍內(nèi)的高精度地層對比格架。

In the term of sedimentary features of Neopaleozoic in south of North China Basin, lateral variation of sedimentary facies was studied selectively in Benxi-Taiyuan Formation, Shanxi Formation, Lower Shihezi Formation, Upper Shihezi Formation and Shiqianfeng Formation. Lithofacies paleographic features and the sedimentary evolutionary process of Late Paleozoic in south of North China Basin were worked also.

根據(jù)華北盆地南部上古生界的沉積特點国产婷婷在线，按本溪組—太原組狼友视频网页、山西組、下石盒子組亚洲综合在线图片、上石盒子組和石千峰組5個層組分別開展了沉積相的橫向變化對比研究，并以此為基礎探討了華北盆地南部晚古生代的巖相古地理特征及其沉積演化過程欧洲最大黄色网站。

Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei palaeohigh s in Tarim Basin;2. The palaeohigh in Junggar basin underwent multistage evolution from Neopaleozoic to Cenozoic, and four basic types such as successional, discontinuous, tilted and thrust ones were developed.

準噶爾盆地古隆起經(jīng)歷了自晚古生代至新生代的多期次演化黄片vs毛片，發(fā)育了繼承型、間斷型97国产精品免费视频、掀斜型和沖斷帶型等4種古隆起基本類型国产嫖娼妓院视频网站，通過構造沉積演化及油氣成藏分析探討了陸梁隆起sansansy.com、莫索灣凸起、車莫隆起的油氣勘探領域和勘探方向亚洲视频二区三区。

By comprehensive analysis of the characteristics of formation and reconstruction, six tectonic belts in the northeast part of Junggar basin were divided: marginal obduction zone in Early Paleozoic(O1-2)?melange mag-ma collision zone of late Paleozoic (D1), volcanic arc-compression zone of Late Paleozoic (D1), back-arc folded belt of Late Paleozoic (D2_3), marginal depression folded belt of Late Paleozoic (C1-P2) and foreland basin gentle anticline belt of Mesozioc era, etc.

通過&建造&與&改造&特征的綜合分析超碰免费欧美自拍，劃分了準噶爾盆地東北緣的構造帶：早古生代（1－2）陸緣逆沖帶；晚古生代（D1）混雜巖漿碰撞帶亚洲激情黄色视频；晚古生代（D1）火山巖漿島弧擠帶www色色；晚古生代（D2－3）弧后盆地褶皺帶；晚古生代（C1－P2）陸緣盆地褶皺帶以及中生代前陸盆地平緩背斜帶等6個構造帶插抽视频。