发育同沉积构造坡折带是断陷盆地的基本特征。
Syndepositional structural slope-break zone is a basic characteristic of rift-subsidence basin.
断层坡折带是油气藏聚集的有利地带，也是陆相断陷盆地隐蔽油气藏勘探的新领域。
The fault slope break is a favorable area of oil accumulation and new target of subtle reservoir exploration in terrigenous fault-depression.
断陷盆地是典型的构造活动型盆地，盆地中各种类型的坡折带均有其发育的构造背景和控制机制。
Faulted basin is a kind of typical tectonic active basin, in which there are various kinds of tectonic slope-breaks controlled by different tectonic backgrounds and mechanisms.
在海相盆地和断陷湖盆中都发育坡折带，并对层序和沉积起重要控制作用，这一观点已得到广泛关注并被普遍接受。
Slope breaks are developed in both marine and rift lake basins, and their controlling impact on sequence and deposition has already been widely concerned and accepted.
库车褶皱冲断带东秋里塔格构造带发育与侧断坡有关的位移转换构造。
In the Kuqa fold-thrust zone, a lateral ramp-related displacement transfer structure is developed in the eastern Qiulitag structural belt.
库车褶皱冲断带东秋里塔格构造带发育与侧断坡有关的位移转换构造。
In the Kuqa fold-thrust zone, a lateral ramp-related displacement transfer structure is developed in the eastern Qiulitag structural belt.
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