foreland basin

The second phase ( Beiliu movement) resulted in northwestward advance of the Yunkai anticlinorium and the foreland basin also migrated toward the northwest side;

第二幕（北流运动）使云开复式背斜向西北推进，前陆盆地亦向西北侧迁移。

There are some differences between the two types of foreland basins: ( 1) The epicontinental foreland basin went through passive continental margin or retro?-arc rift stage during tectonic evolution stage, but the intracontinental foreland basin lacked this period.

它们之间的主要区别表现在：（1）从盆地构造演化上看，陆缘前陆盆地经历了裂谷被动边缘或弧后裂谷阶段，陆内前陆盆地则缺乏这一阶段；

Detailed sedimentary research indicates that Late Jurassic Mohe basin contains the alluvial fan, fan-delta and lacustrine facies, belonging to continental molasse deposits of the foreland basin.

详细的沉积学研究表明：晚侏罗世漠河盆地主要发育冲积扇、扇三角洲和湖泊相沉积，属于前陆盆地的陆相磨拉石部分。

The west sichuan depression a typical Superimposed foreland basin.

川西坳陷属典型的叠合前陆盆地.

The marine flysch deposition of early foreland basin appeared in Indosinian; owing to early Indosinian movement the sand mudstones ( T 2) were folded into mountains, which made the late foreland basin be withered away;

印支期出现早期前陆盆地海相复理石沉积，由于早印支运动使T2砂泥岩揉褶成山，晚期前陆盆地夭折。

Age of Sichuan foreland basin is given.

确定了四川前陆盆地的形成时间.

From the Cretaceous, Tarim basin began the new evolutional stage of foreland basin.

白垩初期始, 塔里木盆期陆盆演阶段.

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.

Early Permian seismically induced soft-sediment deformational structures in Bogda region, Xinjiang: stratigraphic records of earthquakes in the retroarc collisional foreland basin

新疆博格达地区早二叠世软沉积物变形构造：弧后碰撞前陆盆地地震记录

Is Jurassic Chaidamu Basin a Foreland Basin?

柴达木侏罗纪盆地是“前陆盆地” 吗 ?

In the Yanshanian period, with continuous NW-directed propagation of the front of the southeastern Guangxi thrust nappe structure, the Jurassic-Cretaceous foreland basin also migrated continuously in a NW direction.

进入燕山期，随着桂东南逆冲推覆构造前缘不断地向NW方向扩展，侏罗纪&白垩纪时期的前陆盆地也不断地向NW方向迁移。

Therefore , foreland basin becomes the favorable place for reservoir.

前陆盆地成藏条件非常优越.

The Western Sichuan Foreland Basin developed Upper Triassic coal measure source rock, which mainly generated gases.

川西前陆盆地具有丰富的天然气资源,发育上三叠统巨厚的煤系烃源岩, 以生气为主,并发育多套储盖组合.

The shallow faults are the result of extensional fracturing of the overlying strata due to lateral compressional warping deformation ( longitudinal buckle deformation) of the basement ( pre-Mesozoic tectonic layer) in the north of the Tabei uplift in the stage of the Kuqa regenerated foreland basin.

浅层断裂是库车再生前陆盆地阶段塔北隆起北部基底（前中生界构造层）受水平挤压翘曲变形（纵弯变形）导致上覆岩层引张破裂的结果。

Yaken anticline zone controlled by deformation mechanism of foreland basin is characterized by subtle detachment along the formation surface and shows gentle fold.

亚肯背斜带在前陆盆地变形机制控制下，以隐伏的顺层滑脱&推覆为特点，褶皱平缓。

Searching salt diapers and related traps in Kuqa foreland basin is important.

库车前陆盆地勘探程度较低,应注重寻找盐底辟构造,以及与其相关的圈闭.

Classification, sedimentary and structural features of foreland basin are discussed.

对前陆盆地类型划分 、 沉积、构造特征进行了研究.

Author suggest a sedimentary environment of foreland basin or low sinuosity meandering river with strong hydrodynamics and sediment provenance mainly from the adjacent mountain.

表明此时主要为水动力较强的山前盆地、低弯度曲流河的沉积环境，物质主要来自于邻近山地的贫磁性母岩。

Tectonic Significance of Meso-Cenozoic Conglomerate in the South of the West Sichuan Foreland Basin

川西前陆盆地南部中新生代砾岩的构造意义

Make a burlesque of* 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

Foreland basin is rich in oil and gas and foreland thrust fault belt is the focus of current exploration.

前陆盆地的油气资源丰富，前陆盆地的前陆冲断带（山前褶皱&冲断带），是油气勘探的重要领域。

Terrestrial heat flow distribution in Kuqa foreland basin, Tarim, NW China

库车前陆盆地大地热流分布特征

Forty-five samples taken from 53 wells in the Kuqa foreland basin, north Tarim Basin, were selected for thermal conductivity measurement in laboratory, and the original thermal conductivity and formation thermal conductivity column were obtained based on the correction of temperature and porosity.

采集45块岩心样品进行热导率测试，在分析库车前陆盆地的地热场的基础上，通过温度和孔隙度的校正，获得原地热导率和地层热导率柱。

The foreland basin to the north edge of Tianshan refers to Junggar Basin.

天山北侧前陆盆地即准噶尔盆地,该盆地南缘存在严重的超高压异常现象.

To some extent, the facies evolution reflects the tectonic controls on the sedimentation of foreland basin.

东昆南前陆盆地的演化过程在一定程度上反映了构造对沉积的控制作用.

Mesozoic basins are distributed around Tethys and belong to southern foreland basin zone.

在海相沉积之后接受了陆相沉积,中生代盆地环特提斯洋分布,属南前陆盆地带.

Because the foreland basin was a highly subsidence, that it was deposited a hugely Plio-Pleistocene sediments.

由于前陆盆地呈现快速沉降, 因而沉积巨厚的晚上 - 更新世沉积层.

The main tectonic deformation in the Pamir Western Kunlun foreland fold and thrust belt started in Early Pliocene ( about 4.6 Ma ago), and migrated gradually from the orogen to the foreland basin, with the faulting and folding becoming younger and weakened in the basin.

帕米尔&西昆仑北麓前陆褶皱冲断带的主要构造变形时间始于上新世早期（距今约4.6Ma），断层、褶皱的变形时代由山前向盆地逐步变新，变形强度由山脉向塔里木盆地逐步减弱。

The evolvement process of the Longmen Shan foreland basin consist of several stages of thrust belt tectonic load and several stages of thrust belt denudation unload. It can be divided into three tectonic load stages and three denudation unload stages.

龙门山前陆盆地的演化过程是由冲断带若干次构造负载阶段与剥蚀卸载阶段组成的，总体上可以分为三个构造负载阶段和三个剥蚀卸载阶段。

Accommodation Space Evolution and Third-Order Sequence Correlation in the Second-Order Sequence of a Foreland Basin

前陆盆地二级层序内可容纳空间发育演化及三级层序对比