裂谷盆地和拉分盆地形成。
裂谷盆地是夭折的裂谷。
辽河盆地是中、新生代发育起来的裂谷盆地。
Liaohe basin is a rift basin developed in the Mesozoic and Cenozoic.
裂谷盆地的成藏组合类型为前裂谷期潜山油气藏；
Play types of rift basins are:(1)buried hill pools of pre rift stage;
东营凹陷是一个含油气十分丰富的第三纪裂谷盆地。
The Dongying Depression is a Tertiary rift basin with rich petroleum resources.
气候和构造是裂谷盆地地层形成的两个重要控制因素。
Climate and tectonics are the two key controls for the formation of the stratigraphy of a rift basin.
辽河盆地是郯庐断裂系的组成部分，属大陆裂谷盆地。
Liaohe basin is a part of Tanlu rifting system, and it belongs to continental 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。
It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift basin.
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.
新生代裂谷盆地主要沿依兰-伊通和敦化-密山断裂呈线状分布。
Cenozoic rift basin is characterized by linear distribution along Yilan-Yitong fault and Dunhua-Mishan fault.
松辽盆地中生代火山岩特征反映了该盆地为弧后裂谷盆地的性质。
The characteristics of the Mesozoic volcanic rock in the Songliao Basin reflect that this basin is a backarc rift basin.
经断裂分析，太原盆地不是裂谷盆地，而是晚新生代的沉积盆地。
Fault analysis show that Taiyuan basin is sedimentary basin of Late Cenozoic rather than rifted one.
近年来裂谷盆地研究的一个重要进展就是认识到了裂谷过程的多幕性。
The recognition of episodic nature of rifting is considered as a major progress in research of rifted basins in recent years.
南黄海北部坳陷为欧亚大陆东部边缘一系列新生代裂谷盆地中的一个。
The north depression in the southern Yellow Sea basin is one of the Cenozoic rift basins in the east margin of the Eurasian continent.
松辽盆地存在裂谷期前火山岩，之后上地壳脆性伸展发育半地堑裂谷盆地。
In the Songliao basin there occurred pre-rift volcanic rocks. Then brittle extension of the upper crust gave rise to a semi-graben rift basin.
裂谷盆地演化可分为裂谷初始期、深陷期、后裂谷早期和后裂谷晚期阶段。
Evolution of rift basins is divided into rift initiation, rift climax, immediate post-rift, and late post-rift stages.
位于蒙古国中部的尼尔金盆地是一个中生代裂谷盆地，目前仍处于勘探早期。
Located in the middle Mongolia, Nilga Bbasin is a Meso-zoic rift basin and is in the early exploration stage at present.
矿化围岩的沉积组合反映其形成于较深海盆地的环境，为裂谷盆地构造背景。
Sedimentation combination of the surrounding rocks suggests that they are formed in deep ocean basin environment, which belongs to rift valley basin.
渤海湾盆地是中、新生代裂谷盆地与石炭-二叠系残留含煤盆地的复合叠合盆地。
Bohaiwan basin is a composite basin polymerized by a Mesozoic and Cenozoic rift basin and a Carboniferous remnant coal-bearing basin.
新生代，东北地区作为太平洋板块俯冲带的弧后地区，形成了典型的弧后裂谷盆地。
In Cenozoic typical back-arc rift basins are formed in ne China where is the back-arc area of Pacific plate subduction zone.
苏丹裂谷盆地油气藏特征与中国东部渤海湾等盆地的油气藏形成和分布有明显的差异。
The characteristics of rift basins in Sudan are much different from those in the active rift basins of East China.
黔西北地区是一个裂谷盆地构造区，盆地内发育铅锌矿床，矿化受断裂和地层的联合控制。
The northwestern Guizhou Province is located in a rift basin with some lead-zinc deposits controlled by the faults and strata.
东部凹陷北段是辽河盆地的一部分，也有人将其称为裂谷段，具典型的裂谷盆地的发育特征。
The northern section of the East Depression in the Liaohe basin, also called rift section, was developed with typical characteristics of rift basins.
构造运动造就的古地貌在陆相盆地，特别是裂谷盆地对层序形成与发育起着重要的控制作用。
Paleo morphology resulted from tectonic movement controlled the sequence formation and development of continental basins, especially of rift basins.
裂谷盆地半地堑边界正断层的生长可以划分为两种模式：断层简单生长模式和断层生长连锁模式。
The propagation and growth of boundary faults can be divided into 2 types: simple fault propagation pattern and fault growth-linkage pattern.
从微量元素、稀土元素、同位素等方面论证了霍各乞矿田中元古宙为大陆边缘弧后裂谷盆地构造环境。
The studies of microelement, rare earth element and isotope compositions that the Huogeqi polymetallic ore field was formed in rift basin of back arc continental marging during Proterozoic Era.
中三叠个旧组以白云岩、灰岩和泥岩为主，属于个旧-那坡弧后裂谷盆地热沉降背景下形成的沉积序列。
Gejiu Formation in Triassic was mainly comprised of dolomite, limestone and mudstone, belonging to the sedimentary sequences of Gejiu-Napo back-arc rift basin under the regime of thermal subsidence.
结合区域沉积环境确定该蛇绿岩带的构造环境为扩张历史暂短、洋陆转换不彻底、发育于消减带上的弧间裂谷盆地。
On the bas is of the regional depositional environment of the ophiolite zone, it indicates a short-term spreading, the ocean-land transform is not complete, and developed on the interarc rift basin .
东北地区中新生代盆地演化经历早侏罗世裂陷盆地、中晚侏罗世分割式前陆盆地、晚侏罗世末期至白垩纪裂谷盆地及新生代裂谷盆地四个演化阶段。
Basin evolution in ne China goes through four stages: early Jurassic rift basin, middle-late Jurassic partitioned foreland basin, late late Jurassic-Cretaceous rift basin and Cenozoic rift basin.
变质玄武岩的地球化学特征与大陆裂谷型火山岩一致，形成于活动陆棚裂陷（谷）盆地的构造环境。
The geochemical characteristics of the metabasalt agree with those of continental rift type volcanic rocks, forming a tectonic environment of the active shelf rift basin.
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