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