The magma is probably generated by rifting.
岩浆的形成可能与裂谷作用有关。
The Bohai bay Basin is a Cenozoic rifting one.
渤海宵盆地是一个新生代裂陷盆地。
Rifting basins and pull-apart basins were formed.
裂谷盆地和拉分盆地形成。
Rifting played an important role in formation of the back arc basins.
裂陷作用也控制着弧后盆地的形成。
Liaohe basin is a part of Tanlu rifting system, and it belongs to continental rift basin.
辽河盆地是郯庐断裂系的组成部分，属大陆裂谷盆地。
Both Etna and Tharsis show similar patterns of rifting running through the body of the volcano.
不管是埃特纳火山还是塔西斯高地，贯穿火山山体的裂隙也都显示出了相似的格局。
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。
Post rifting regional uplift resulted in low maturity of source rock and wide difference from each other.
裂谷期后的区域抬升作用导致烃源岩的成熟度偏低，并且各断陷之间有机质的热演化程度相差悬殊。
NE China experienced regional rifting, post-rifting thermal subsidence and thermal reverse in Late Mesozoic.
中国东北晚中生代经历了区域性的裂谷期、后裂谷热沉降期和反转期。
Complicated tectonic styles and geological structures were generated by multi-episodic rifting and inversion.
多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构。
The other intrusive bodies are post-orogenic granitoid in association with the continental uplifting and rifting.
其余各岩体是本区造山后与大陆抬升作用以及大陆裂谷作用有关的花岗岩类。
The recognition of episodic nature of rifting is considered as a major progress in research of rifted basins in recent years.
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 forming and distribution of the structural fractures are related to the local tectonics (e. g. the rifting and the folding).
构造裂缝的形成和分布与局部构造作用(断层、褶皱作用)有关。
The structural belt at the north foot of the Mountain Funiu consists of the Luonan-Luanchuan rifting zone and the Shirenshan block.
伏牛山北麓构造带包括洛南-栾川断裂带和石人山地块。
Basin development in Bobal Bay comprises two periods, i. e. rifting and depression, during which very thick Tertiary sequences deposited.
渤海湾盆地经历了断陷和拗陷两个发育阶段，其间接受了巨厚的第三纪沉积。
There have four kind of basins in the South China Sea area: rifting basin, strike-slip rifting basin, fore-land basin and fore-arc basin.
南海地区新生代沉积盆地有四类：张裂盆地、走滑拉张盆地、前陆盆地和前弧盆地。
The rifting and paleokarst are the main factors that controlled the distribution of reservoir, the favored areas of reservoir are banding.
断裂作用和古岩溶作用是控制储层形成分布的主要因素，有利的储层分布区域主要以条带状分布。
The east depression of Liaohe Basin is a Cenozonic intra continental rifting basin formed on the late Cretaceous Paleocene regional uplift.
辽河盆地东部凹陷是在晚白垩世—古新世区域隆起背景上形成的新生代板内裂陷。
The two tectonic systems are concrete manifestations of the active rifting and passive rifting mechanisms in the basin during the Cenozoic.
这两种构造系统是盆地区新生代时期主动裂陷和被动裂陷两种作用机制的具体表现。
The latter can be subdivided into 4 stages, including initial rifting, intense rifting, late rifting and Late Tertiary integral downwarping.
新生代裂陷盆地旋回又划分为早期裂陷、强烈裂陷、晚期裂陷和晚第三纪整体坳陷4个阶段。
This four-element architecture may be caused by a regional stress field evolution from rifting, sagging to differential inversion uplifting.
这种四元结构的形成，起因于区域构造应力场转变成裂陷作用、拗陷作用和差异隆升反转作用的演化。
The developments of those two types of sequences are the sedimentary and stratal response to the basin dynamics of the Songliao basin at rifting time.
这两种不同类型的层序发育正是松辽盆地断陷阶段盆地动力学机制的沉积、地层响应。
Recent studies have further improved our understanding of basin forming mechanism in deep processes, combined mechanism and multiple rifting and inversion.
盆地形成机制研究在深部过程控制、多重机制联合作用、幕式裂陷和反转过程等方面取得显著进展。
The metallogenetic environment is a closed bathyal-abysmal basin and the metallogenetic setting is a rifting with characteristics of "ocean basin evolution".
成矿环境为半深水一深水局限盆地，成矿背景是以“洋盆化”为特征的裂谷作用。
Geochemical and stratigraphical studies suggest that the tectonic setting of the Gangdese region is depressional rifting to the northern margin of Gondwanaland.
岩石地球化学示踪和地层学研究表明，冈底斯带石炭纪为伸展背景下的冈瓦纳陆缘裂陷环境。
The East China sedimentary basins are believed to be formed by extension rifting simultaneously with the process of uplifting, subsiding, faulting and deposition.
我国东部沉积盆地是在引张背景下形成的。盆地中边隆起、边沉降、边断裂、边沉积，构造作用与沉积作用同步发生。
Bozhong depression with vastly thick Tertiary System deposit underwent two evolution stages of structure-deposit: rifting stage and post-rifting depression stage.
渤中坳陷的构造—沉积演化经历裂陷和裂后坳陷两大阶段。
While, later rifting stage was divided two evolutionary stages which were from Guantao group to Ming-2 member and from Ming-1 member to Quaternary sedimentary period.
新近纪-第四纪的后裂陷阶段可分为二个演化阶段，即馆陶组-明二段和明一段-第四系沉积时期。
During the period from Late Oligocene to Middle Miocene, the basin changed from rifting to depression, and the depositional area continued to expand in the Marine environment.
晚渐新世—中中新世，盆地逐渐由断陷转为断拗，沉积范围不断扩大，整体处于海相沉积环境。
These are proper rear boundaries of continental margins, the geodynamics of which are characterized by rifting on shelves, continental slopes, and marginal oceanic depressions.
它们位于大陆边缘区的后缘，其地球动力学作用以大陆架、大陆斜坡和边缘海沉降区域的裂谷作用为特征。
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