鄂尔多斯盆地是叠加在华北古生代克拉通台地之上的中生代大型陆内盆地。
The Ordos basin is a large Mesozoic intracontinental basin superimposed on the Paleozoic North China craton.
盆地构造演化经历了前陆盆地和陆内盆地两个大阶段，后者又进一步分为陆内裂谷时期、再生前陆盆地时期和盆地消亡时期。
It has two tectonic evolutionary stages of foreland basin and intracontinental basin that is further divided into three periods of intracontinental rift, newborn foreland basin and dying out basin.
前陆冲断带是前陆盆地内油气聚集的主要场所，也是油气勘探中最难的领域。
Foreland thrust belt is the primary region for the petroleum assemble in the foreland basin, which is the most difficult fields in the petroleum exploring.
最后，作者展望了层序地层学在陆相沉积盆地内砂岩型铀矿找矿中的应用前景。
Finally, the authors look ahead the application potential of sequence stratigraphy to the prospecting for sandstone type uranium deposits in continental depositional basins.
前者为陆内裂陷沟-弧环境产物．后者形成于陆缘盆地构造环境。
The former is formed in trench - arc environment ofintracontinental rift, and the latter in marginal basin.
研究结果表明，前陆盆地内发育有两种层序模式，即构造层序和气候层序。
Two kinds of revolutionary models for sequences including structural sequence model and climate sequence model developed in foreland basin were presented.
在白垩纪后期，地质资料表明这些浅海都从大陆退回到主要的海洋盆地内了，没有人明白为什么。
At the end of the Cretaceous, the geological record shows that these seaways retreated from the continents back into the major ocean basins. No one knows why.
迈卢特盆地是苏丹东南部中—新生代的一个大型陆内裂谷盆地。
Melut Basin is a large-scale basin of the Cretaceous-Paleogene sediment in the southeastern Sudan.
包括隆起带上，仅（内）陆架盆地风暴浪基面之下中心位置有少量灰质白云岩和白云岩沉积。
Limestone deposited in the whole inner shelf basin, including the swell belt, excepting a small mass of dolostone or dolomitic limestone could deposit in the center of basin.
导致右江盆地由陆内裂陷盆地向被动陆缘裂谷盆地演化。
It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift basin.
塔里木盆地自二叠纪以来，历经盆地扩张和盆地俯冲以及陆内造山作用的过程。
Since the Permian, the Tarim Basin had undergone basinal extension, subduction and intro-continental orogeny.
陆内俯冲前陆盆地发育在南缘西部。
The inland subduction basin was developed in the west of southern basin.
与弧背前陆盆地和周缘前陆盆地相并列，并对应于板块构造演化历程中的大洋消减、大陆碰撞和陆内缩短三个不同性质的聚敛阶段。
Therefore they are corresponding to the three different featured convergent stages of ocean subduction, continental collision and intra-continent contraction in the structural evolution of plates.
与弧背前陆盆地和周缘前陆盆地相并列，并对应于板块构造演化历程中的大洋消减、大陆碰撞和陆内缩短三个不同性质的聚敛阶段。
Therefore they are corresponding to the three different featured convergent stages of ocean subduction, continental collision and intra-continent contraction in the structural evolution of plates.
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