沉积环境为被动大陆边缘。
The sediment environment was in the passive continental margin.
震旦纪是塔里木盆地被动大陆边缘盆地重要发育期。
Sinian is one of the most important stage of development of passive continental margin basin in Tarim Basin.
伸展区剥离断层模式同样适用于被动大陆边缘的形成和演化。
Detachment models can also applied to the formation of passive continental margins.
陆相层序地层与被动大陆边缘海相层序地层之间存在较大的差异。
Sedimentation in continental basins has been controlled by many factors and the main control factors in basins of different types are not the same.
碎屑物常量化学成分投点表明，其形成时构造背景属被动大陆边缘。
The data of chemical composition of sediments indicate that the tectonic background of the turbidites is passive continental margin environment.
因此提出了库鲁克塔原洋裂谷和满加尔初始被动大陆边缘的新见解。
Therefore, the Kuruktag ur-ocean rift and Manjaer original continental margin were proposed.
南海是西太平洋地区最大的边缘海之一，其北部具有被动大陆边缘特征。
The South China Sea is one of the largest marginal seas in the western Pacific region, with its northern margin being characterized by a passive continental margin.
皖南地区的江南隆起带，在震旦纪—中三叠世与周边一样处于被动大陆边缘海相环境。
Like surrounding areas, the Jiangnan uplift belt in southern Anhui was situated on a passive continental margin during Sinian to Middle Triassic.
在空间上有成带分布特点，主要分布在裂谷带和被动大陆边缘，与同生断裂密切相关。
These ore deposits displaying belteddistribution mainly occurred in rift and passive continental margins, related to the syndepositional fractures.
四川盆地西部在晚三叠世早期（卡尼期）为被动大陆边缘环境， 沉积岩石单元为马鞍塘组。
The Maantang Formation in western Sichuan basin was probably located in the shelf of the passive continental margin in Upper Triassic.
对应每一旋回，喀喇昆仑地层区和塔里木地层区发育有被动大陆边缘盆地和碰撞造山两种类型的岩石组合。
For Kala Kunlun and Tarim, two kinds of rock associations, passive continental marginal basin and collision orogenic belt, are developed corresponding to each cycle.
依据起源于被动大陆边缘海相盆地的层序地层学基本原理，对缺乏地形坡折的柴达木盆地第四系进行了层序地层研究。
The Quaternary of Qaidam basin, being lack of topographic break, was studied based on the theory of sequence stratigraphy, which originated from marine basins in passive continental margin.
通过对西非被动大陆边缘结构、构造特征，以及边缘发育演化简史的分析，探讨了西非被动大陆边缘形成演化的动力学背景。
Based on the analysis of the structure and the brief evolution history of the passive continental margin in West Africa, the dynamic background of formation and evolution of the margin is discussed.
南海北部被动大陆边缘是板块活动相对较弱的地区，业已证实是巨大天然气田形成的有利场所，同时也是水合物发育的有利地区。
The plate activity is weaker in the passive continental margin of the northern South China Sea, which is favorable for forming the large-scale gas field and gas hydrate reservoirs.
南海北部被动大陆边缘是板块活动相对较弱的地区，业已证实是巨大天然气田形成的有利场所，同时也是水合物发育的有利地区。
The plate activity is weaker in the passive continental margin of the northern South China Sea, which is favorable for forming the large-scale gas field and gas hydrate reservoirs.
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