1)foreland basin前陆盆地
1.Transporting conditions of faults required in formation of large and medium gas fields with high efficiency in foreland basin;前陆盆地高效大中型气田形成的断裂输导条件
2.Different origins of natural gas in secondary gas pool in Western Sichuan foreland basin;川西前陆盆地次生气藏天然气来源追踪
3.Overpressure compartment sealed by faults in Kuqa foreland basin;库车前陆盆地断裂封存的超高压封存箱
英文短句/例句
1.Is Jurassic Chaidamu Basin a Foreland Basin?柴达木侏罗纪盆地是"前陆盆地"吗?
2.Discussion of Depositional Filling and Sequence Stratigraphy Model of Continental Foreland Basin:Taking the Kuqa Foreland Basin as an Example陆相前陆盆地沉积充填与层序地层模式探讨——以库车前陆盆地为例
3.THE BASIN-MOUNTAIN COUPLING RELATION IN THE FORELAND BASINS IN CENTRAL CHINA中国中部前陆盆地盆山耦合关系分析
4.GEOCHEMICAL IDENTIFICATION OF THE DEVONIAN FORELAND BASIN IN THE EASTERN QINLING,THE SOUTHERN SHAANXI陕南东秦岭泥盆纪前陆盆地的地球化学鉴定
5.The Relationship between Tectonic Evolution of Intracontinental Foreland Basin and Oil-gas in Southern Magin of Junggar Basin;准噶尔盆地南缘陆内前陆盆地构造演化与油气关系
6.The Analysis of the Poolforming Features in the Upper Triassic Xujiahe Formation of Western Sichuan Foreland Basin川西上三叠统前陆盆地成藏特征分析
7.SOUTH QINLING IN THE DEVONIAN:JUXTAPOSITION OF PERIPHERAL FORELAND BASINS AND NEW-BORN OCEANIC BASINS南秦岭泥盆纪:周缘前陆盆地和新生海洋盆地并列
8.Tarim basin is a huge superposed basin composed of Paleozoic cratonic basin and Meso-Cenozoic foreland basin.塔里木盆地是一个由古生代克拉通盆地与中、生代前陆盆地叠合而成的大型叠合盆地。
9.The Sedimentary Facies in Marginal Foreland Basin of Triassic Age in Southwestern Guizhou黔西南地区三叠纪周缘前陆盆地沉积相特征
10.Some key tectonics characteristics of Chinese foreland basins and their petroleum exploration中国前陆盆地构造地质特征综述与油气勘探
11.Sequence-based Lithofacies and Paleogeographic Characteristics of Upper Triassic Xujiahe Formation in Sichuan Basin四川类前陆盆地须家河组层序—岩相古地理特征
12.Western Sichuan Depression is a foreland basin developed in the west of Sichuan basin since late Triassic.川西坳陷是指四川盆地西部晚三叠世以来形成的前陆盆地。
13.From the Cretaceous, Tarim basin began the new evolutional stage of foreland basin.从白垩纪初期开始,塔里木盆地进入晚期前陆盆地演化阶段.
14.The Research on Characteristics and Reservoir of Foreland Basin of Western Margin of Ordos Basin;鄂尔多斯盆地西缘前陆盆地构造特征和油气成藏研究
15.Depositional setting and evolution of the Paleogene-Neogene foreland basin of southern margin of Junggar Basin准噶尔盆地南缘古近纪—新近纪前陆盆地沉积格局与演变
16.Himalayan movement made the area developed as a para-foreland basin.喜马拉雅运动使本区发育为类前陆盆地。
17.The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny.前陆盆地的终结标志着碰撞造山作用的结束。
18.Qinling polygenic foreland basin in Late Caledonian to Early Variscan秦岭加里东晚期—华力西早期复式前陆盆地
相关短句/例句
forland basin前陆盆地
1.Based on forland basins evolution,tectonic features,sedimental model,thermal process,reform process and model recovery,the paper analyzes forland basins theories and pays more attention to geological process,evolutional development and sedimental model.阐述前陆盆地理论进展;对前陆盆地的成因演化历史、结构特征、充填特征、热历史演化、后期改造及原型恢复等方面作了综合分析;全面探讨前陆盆地的地质过程、成因演化机理和充填特征;在对比断陷盆地的基础上提出了前陆盆地各个方面及地质过程的特征和进展。
3)palaeo-foreland basin古前陆盆地
1.According to the latest researches, there is a set of Mesozoic(T_3-J_(1+2)) palaeo-foreland basin deposits in the deep-seated Songliao Basin, which are composed of detrital rock, coal and volcanic rock.根据最新的研究成果,松辽盆地深层存在一套早中生代(T3-J1+2)含煤和火山岩的古前陆盆地沉积。
4)paraforeland basin类前陆盆地
5)Bi-foreland basin双前陆盆地
6)intracontinental foreland basin陆内前陆盆地
1.Geological characteristics and hydrocarbon potential between epicontinental and intracontinental foreland basins;陆缘和陆内前陆盆地主要特征及含油气性研究
2.The Relationship between Tectonic Evolution of Intracontinental Foreland Basin and Oil-gas in Southern Magin of Junggar Basin;准噶尔盆地南缘陆内前陆盆地构造演化与油气关系
延伸阅读
前陆盆地前陆盆地fore-landbasin介于克拉通与造山带前缘的沉积盆地。又称山前坳陷、前渊。前陆是指克拉通与冒地斜相邻的部分。前陆盆地按其形成的构造位置可以分为两类：①周边前陆盆地，紧靠在大陆碰撞所产生的造山带外侧，在向下挠曲的陆壳之上形成沉积盆地。如中国天山北麓山前坳陷，喜马拉雅山南麓印度河-恒河盆地和阿尔卑斯山北麓磨拉石盆地。②弧后前陆盆地，发育在岩浆弧之后，常与B型俯冲有关，当断层片叠覆于陆壳上形成荷载时，区域性的均衡沉降产生前渊，聚集大量来自前陆和后陆方向的沉积物，如加拿大阿尔伯达盆地。前陆盆地的发育主要与冲断层带的活动有关，由于冲断带荷载使岩石圈挠曲，形成前陆沉降。因此前陆盆地演化主要与冲断带向克拉通方向推进有关。当盆地位于活动冲断带前方时，称为前缘盆地。随着冲断带的推进，盆地就位于冲断层的顶部，称为冲驮盆地。前陆盆地的沉积作用在早期与晚期不同，早期沉积物通常为海相细粒的浊流沉积，称为复理石盆地，后期沉积物主要为浅水或陆相冲积扇或扇-三角洲粗碎屑沉积，称为磨拉石盆地。从岩石学特征来看，前陆盆地的早期沉积中石英矿物丰富，而长石矿物较少，说明物源主要来自克拉通，后期沉积中含有较丰富的岩屑，说明物源主要来自造山带，由于造山带逐步遭受剥蚀，在沉积的碎屑物中出现倒序现象，如年代较老的砾岩层，其源岩时代较新，而年代较新的砾岩层，其源岩时代较老。因此前陆盆地的构造活动与沉积作用具有相关性。
