The sediment environment was in the passive continental margin.
沉积环境为被动大陆边缘。
There is potential for petroleum exploration around the Manjaer original continental margin.
环满加尔初始大陆边缘具有良好的油气勘探前景。
Therefore, the Kuruktag ur-ocean rift and Manjaer original continental margin were proposed.
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。
The eastern China continent has entered into the stage of rifting continental margin since Oligocene.
自渐新世，中国东部大陆进入了张裂的大陆边缘阶段。
This paper deals with the features of late Middle Proterozoic active continental margin in South China.
本文阐述了华南中元古代晚期活动陆缘特征。
In the light of the sedimentary tectono-geochemistry of they formed in shallow sea of continental margin.
硅质岩沉积大地构造地球化学表明硅质岩的沉积环境是大陆边缘的浅海。
It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift 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。
The forming mechanism of the volcanic rocks has been illustrated by surge tectonics of continental margin.
文章还提出大陆边缘涌动构造用以解释其形成机制。
The relationship between sporopollen assemblage and vegetation of the continental margin has been discussed.
深入探讨了南海东北部表层沉积孢粉分布格局与陆缘植被的关系。
The major disruption of Heigou-Luanchuan has determined the active continental margin of the ancient north China plate.
黑沟一栾川大断裂，限定了古华北板块南部活动大陆边缘的边界。
Baoyintu Group is recognized as an ancient fragment from crystalline basement in stage of continental margin disjoined.
宝音图群为陆缘拉张解体阶段源自结晶基底的裂解古陆块。
Canyon and channel can be good reservoir of hydrocarbon have been proved by the well drilling on passive continental margin basins.
峡谷水道可以作为粗粒沉积物的最终沉积场所，已被钻探证实可作为良好的油气储集体。
The Maantang Formation in western Sichuan basin was probably located in the shelf of the passive continental margin in Upper Triassic.
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 passive continental margin is a comparatively weak region of plate tectonic movement, but it is a favorable region for gas hydrate.
非活动陆缘是板块活动相对较弱的地区，也是水合物发育的有利地区。
There are various indications that the Liuling Group belongs to the stable continental margin deposits of the north of the Yangtse plate.
冬种迹象表明，刘岭群应属扬子板块北部的稳定大陆边缘沉积。
Tectono -sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、弧后裂谷和拗陷盆地。
Tectono - sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、后裂谷和拗陷盆地。
Located in middle part of the Jinshajiang tectonic belt, the Yangla copper orefield was in the clinoform area of an active continental margin.
滇西羊拉铜矿区位于金沙江构造带中部，当时处于活动大陆边缘的半深水斜坡之上。
The data of chemical composition of sediments indicate that the tectonic background of the turbidites is passive continental margin environment.
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。
Like surrounding areas, the Jiangnan uplift belt in southern Anhui was situated on a passive continental margin during Sinian to Middle Triassic.
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。
Southeastern China continental margin has undergone a complicated convergence process of the Eurasian plate with the Pacific plate and Tethys plate.
中国大陆东、南边缘经历了欧亚板块与太平洋板块和特提斯板块会聚作用的复杂过程。
Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic.
断裂和断块构造是南海北部陆缘新生代构造作用的基本特征。
The geochemistry of the cherts reflects that the cherts coexisting with island-arc volcanic rocks all formed the background of continental margin basin.
硅质岩的沉积地球化学研究表明，与岛弧火山岩共生的硅质岩为生物成因，形成于大陆边缘盆地的构造背景。
This is apparently related to the tectonic setting of Shandong, namely, the continental margin where the Pacific Plate collided against the Eurasian Plate.
之所以如此，显然与山东所处的大地构造位置，即太平洋板块与欧亚板块相互碰撞的陆缘地带密切相关。
Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.
根据基底性质分析，探讨了东海大陆边缘新生代沉积盆地的形成演化与成因机制。
The South China Sea is a huge marginal sea at East-Asian continental margin, and a tectonic region of the transitional crust type from continental to oceanic.
南海是东亚大陆边缘的巨型陆缘海，属大陆—大洋过渡型地壳构造区。
According to the isotopic dating, it was emplaced into the active continental margin in Permian, which was resulted from the eastward subduction of the Tethys sea.
结合同位素测年结果及其它地质事件，确定是在二叠纪侵位于活动陆缘，是区内古特提斯洋向东俯冲消减作用的产物。
According to the isotopic dating, it was emplaced into the active continental margin in Permian, which was resulted from the eastward subduction of the Tethys sea.
结合同位素测年结果及其它地质事件，确定是在二叠纪侵位于活动陆缘，是区内古特提斯洋向东俯冲消减作用的产物。
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