裂陷盆地

渤海湾新生代裂陷盆地的伸展模式及其动力学过程

Extensional pattern and dynamic process of the Cenozoic rifting basin in the Bohai Bay

裂陷盆地构造-热演化模拟

Tectonic-thermal modeling of rifting basin

第一期盆地（J（1＋2））为断陷盆地；第二期盆地（J3－K）为NE向分布的裂陷盆地群。

The first - stage basins ( J_ ( 1 + 2 )) belonged to faulted basins , and the second - stage basins ( J_3 - K ) were rift basin group with NE strike .

太平洋板块作用阶段（E-Q），包括伸展裂陷盆地阶段（E）及坳陷萎缩盆地阶段（N-Q）。

The action stage of the Pacific plate ( E-Q ), including the stage of rift-basin ( E ) and depression consumption ( N-Q ) .

大型裂陷盆地深层具有良好的油气成藏条件。

Large deep rift basin has good conditions for hydrocarbon accumulation .

渤海宵盆地是一个新生代裂陷盆地。

The Bohai bay Basin is a Cenozoic rifting one .

粤北泥盆纪裂陷盆地特征及其演化

Characteristics and evolution of Devonian rift basin in northern Guangdong

地幔面起伏的调整结束了裂陷盆地的发育。

The adjustment of mantle surface relief ended the rift basin development .

裂陷盆地断层的形成和演化&目标砂箱模拟实验与认识

Fault Formation and Evolution in Rift Basins & Sandbox Modeling and Cognition

裂陷盆地控制了石炭系烃源岩，使其沿裂陷槽分布；

The aulacogen basin controlled the Carboniferous source rock distributed along rift valley .

基底先存构造对裂陷盆地断层形成和演化的控制作用规律

The law of basement pre-existing fabric controlling fault formation and evolution in rift basin

后期裂陷盆地的形成。

The later formation of the split basins .

华北裂陷盆地不同块体地壳结构及演化研究

Research on the crustal structure and evolution of different blocks in North China rift-depression basin

松辽盆地是一中生代形成的伸展裂陷盆地。

Songliao Basin is a expanding and rifted basin which was formed in Mesozoic era .

伊犁盆地是发育在晚古生代火山裂陷盆地基础之上的中生代拗陷盆地。

Yili basin is a Mesozoic down-warped basin superimoposed on the late Paleozoic volcanic taphrogenic basin .

第四类为东部走滑拉张裂陷盆地的混合成因生物天然气藏；

The forth are mixed-genetic biogas pools in the eastern strike-slip extensional rift basins of China .

复理石的沉积作用发育在裂陷盆地年青底板上的看法被广泛接受。

The deposition of flysch onto the young floors of chiasmic basins is widely accepted as certain .

这种相当年轻的裂陷盆地的高热流是由岩石圈冷却所引起的。

In the case of sufficiently young chasmic basins high heat flows are due to lithospheric cooling .

中侏罗世克拉通边缘坳陷盆地、白垩纪弧前盆地和晚白垩世末&新生代弧后裂陷盆地等3个构造演化阶段。

- Middle Jurassic depression on a cratonic margin , Cretaceous forearc basin and Latest Cretaceous-Cenozoic backarc basin .

瓯江凹陷是东海陆架弧后裂陷盆地的一部分。

Again , the depression is a part of the backarc rifted basin on the East China Sea shelf .

发育于蒙古弧形褶皱带的中生代沉积盆地群可分为残余海盆地、前陆盆地、裂陷盆地三种类型。

The Mesozoic basins of Mongolia can be classified into residual sea basins , foreland basins and rift basins .

其地层序列反映了弧后裂陷盆地从形成到消亡的过程。

Its stratigraphic succession reflects the evolution of the back - arc rift basin from starting to the end .

普通意义上的“裂谷”、裂陷盆地实际上大部分是一系列半地堑以不同方式联结而成。

Most of the rifts and faulted basins , in common sense , are series of halfgrabens connected in different ways .

油气藏的类型主要受控于裂陷盆地的伸展程度、同生断层及沉积相带。

The types of hydrocarbon pools are mainly controlled by the extension of rifted basin , contemperaneous faults and sedimentary facies .

裂陷盆地内没有发现前更新世沉积物，该裂陷带断开了上新世地层和5.45Ma的白云母花岗岩体。

There are no pre-Neogene sediments in the basin , which cuts Pliocene strata and a two-mica granite of 5 . 45 Ma .

各幔枝构造（造山带）间具有明显的可比性，并共同与中心裂陷盆地构成盆-山耦合关系。

Here the mantle branch structures ( orogens ) can be compared with one another and are coupled jointly with the central rifting basin .

渤海位于渤海湾新生代裂陷盆地的东部。

The Bohai Sea is located in the east of the Bohai Bay Cenozoic rift basin , and has been characterized by intense tectonic activities since Quaternary time .

柴达木第三纪转换裂陷盆地形成演化主要受控于地幔热柱的形成和衰减作用，同时喜马拉雅运动等运程应力作用对盆地的演化至关重要。

The formation and evolution of the basin are considered to be constrained by the formation and waning of mantle plumes and stress processes of the Himalayan orogeny .

深水油气的成藏模式，除裂陷盆地的成藏模式外，还有裂后热沉降期裂陷的深水浊积砂岩油藏、底辟构造油藏等特殊类型。

TECTONIC-THERMAL MODELING OF RIFTING BASIN The hydrocarbon reservoirs preserved in the various trap in the rifting basin , and some unique deepwater turbidite sandstone , and diapir structures .

通过对华北裂陷盆地内不同块体的深地震测深资料处理，得到与构造演化过程相关的、不同性质块体的地壳结构特征。

Crustal structures of blocks with different features associated with tectonic evolution process are got by processing of DSS data of different blocks within the North China rift depression basin .