The sediments deposited in the rifting and the early depression stages provided materials and fluids for ancient oil reservoirs and ore deposits. 右江盆地裂陷期和坳陷早期的沉积物提供研究区金矿与古油藏的物质与流体。
Periodic Rifting Activity and Its Controlling on Sedimentary Filling of Paleogene Period in Nanpu Sag 南堡凹陷古近纪幕式裂陷作用及其对沉积充填的控制
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。
Features of paleogene episodic rifting in Huizhou fault depression in the Pearl River Mouth basin 珠江口盆地惠州凹陷古近纪幕式裂陷特征
The basin and the mountain were formed by Cenozoic rifting on the basis of the North China peneplain, which was formed in the Late Cretaceous. 盆地和山脉是在晚白垩世形成的华北准平原上经新生代裂陷作用产生的。
In the Songliao basin, a network of normal faults, characterized by relative variability in strike and short length, was widely produced in sediments accumulated during the early post rifting. 在松辽盆地后裂谷早期的沉积地层里广泛发育着一个长度相对短、走向变化相对大的正断层系。
Late Permian to Triassic rifting and subsidence resulted in the deposition of as much as9 kilometers of Triassic strata, locally injected with sills. 二叠纪晚期到三叠纪断裂和下沉作用形成了大约9千米厚的第三纪沉积地层,在其中有岩床的切入。
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。
Qing-Yuan district is a granite-greenstone terrain, The greenstone was formed during the youth stage of massif rifting in late Archean. 花岗岩形成巨大的岩体。清原地区是一个花岗&绿岩区,绿岩是在晚太古代年轻地体裂谷期形成。
Since tha latest of cretaceous, the xiihu sag had been undergoing rifting stage during the Paleocene and the eocene, inversion stagc during the Oligocene and the miocene, and regional subsidence stage during the Pliocene and the quaternary. 晚中生代末期以来,经历了古新世-始新世的裂谷盆地阶段。渐新世-中新世的盆地反转阶段和上新世-第四纪的区域沉降阶段。
The Bohai bay Basin is a Cenozoic rifting one. 渤海宵盆地是一个新生代裂陷盆地。
Discussion of Basin-fill Mechanism during Eogene Rifting Phase in Oujiang Trough, the East China Sea 东海瓯江凹陷早第三纪裂谷期盆地充填机制探讨
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 magma is probably generated by rifting. 岩浆的形成可能与裂谷作用有关。
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。
According to geological and geophysical data, kinematic system of this rifting is discussed. 根据地质和地球物理资料探讨了这期裂陷作用的运动学体制。
Episodic Rifting Dynamic Process and Quantitative Model of Mesozoic-Cenozoic Faulted Basins in Eastern China 中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型
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。
We believe that there were platform sediments in the Paleozoic and the rifting depression sediments from Mesozoic to Cenozoic in the Yellow Sea area. 对南、北黄海沉积盆地形成的构造背景和盆地的构造类型进行了研究,认为在古生代它们是台地相沉积,中生代和新生代是张裂盆地;
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。
From the Cretaceous Period to the Cenozoic Period, the volcanism was mainly related to the rifting; 从白垩纪至新生代,火山作用主要与裂谷作用有关。
During rifting folding and inversion, gold-bearing metamorphic hydrothermal fluid and gold mineralization formed; 在裂谷褶皱、回返期,形成含金变质热液,形成金矿化;
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。
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。
Jinchuan nickle copper deposit was formed during the early stage of the rifting process of the paleo continental margin; 金川镍铜矿床形成于古大陆边缘的裂谷环境早期;
Our observations are consistent with rifting, lithospheric thinning, and mantle upwelling in the region. 研究结果表明与这些地区裂谷、岩石圈减薄和地幔上涌区相一致。
There are many rifting basins in the north margin; 北部和西部边缘上发育着张性沉积盆地和走滑拉张盆地;
The South Block is rifting toward southeast with strata inclining to southeast in general. 南块体朝东南方向断陷,岩层总体朝东-南方向倾斜。
Tectonic activities controlled basin type, subside central rifting, source rock distribution, oil and gas migration and accumulation as well. Furthermore, it controlled trap formation and petroleum distribution. 研究区的构造活动不仅控制了沉积盆地类型和沉降中心的迁移,而且控制了烃源岩的分布、油气运移和聚集,还影响了圈闭的形成和油气分布。