万安盆地是南海西南部陆架上的大型新生代沉积盆地。
Wan 'an basin is a large scale Cenozoic sedimentary basin which is located on southwest shelf of the south China Sea.
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。
Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.
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。
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.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
花海凹陷是一个小型的中新生代沉积断陷，其油气成藏条件在中小型盆地中具有代表性。
Huahai sag is a small sedimentary fault-depression basin formed during Mesozoic-Cenozoic periods, its accumulation conditions of oil and gas represent the characteristics of medium-small basins.
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.
活动性强、深部作用活跃，是中国沉积盆地，特别是中、新生代盆地的两个重要特点。
Strong activity and active deep action are two important features of Chinese sedimentary basins, especially for Meso-Cenozoic basins.
根据胶莱盆地区域地质特征，地球动力学背景及盆地中、新生代沉积特征分析，论述盆地的发育和演化阶段，并对胶莱盆地含油气前景进行探讨。
The evolution features of the Jiaolai Basin are discussed in this paper on the basis of its regional structure, geodynamic background and sedimentary features of the Mesozoic and Cenozoic.
川东北地区是一个具有复杂构造的中新生代盆地，以海相沉积为主的三叠系是重要的储层。
Abstract1 Northeast Sichuan basin is a Mesozoic-Cenozoic basin with complex tectonics, Triassic formation based on Marine deposits was an important potential resource and reservoir.
廷贾断裂的掀斜作用使曾母盆地和文莱盆地沉积了巨厚的新生代沉积物。
It is due to the development of Tingjia fault that the thick Cenozoic sediments might be deposited in basins of Zengmu and Wenlai.
与现代叠层石的对比进一步明确了新生代柴达木盆地湖相叠层石的沉积特点和属性特征。
Compared with the modern stromatolites, the Neogene stromatolites in the Qaidam Basin was further elucidated in sedimentation and features.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
新生代盆地构造和沉积分布特征表明渤海湾盆地是一个中、新生代叠合盆地。
The characteristics of structure and depositment in this Mesozoic and Cenozoic time show that Bohai basin is a Mesozoic and Cenozoic composite basin.
许多中—新生代盆地沉积充填中铀矿化显著，有机质丰富，铀矿与有机能源同盆共存，铀矿化与有机质内在关联备受关注。
Uranium mineralization is commonly associated with organic matter in many Meso—Cenozoic basins, and their intrinsic relationship is an interested subject to many ore deposit researchers.
这些盆地中有着巨厚的中、新生代的沉积，具备了良好的生油与储油条件。
In these basins, there are Meso-Cenozoic thick sediments, with favourable conditions for the formation and accumulation of petroleum.
叶城盆地属于塔里木盆地的西南坳陷，在晚新生代沉积了巨厚的磨拉石建造。
The Yecheng foreland basin is a part of the southwest sag of the Tarim Basin and contains late Cenozoic molassic deposits with great thickness.
南襄盆地是中新生代含油气沉积盆地，它们形成演化与断裂活动密切相关。
Nanxiang basin is a Mesozonic and Cenozonic Era deposit basin which contains oil and gas, its formation and evolution has close relation to faults activity.
本文指出东海盆地是一个大型的以新生代沉积为主的盆地，沉积岩厚度超过万米。
This article indicates that east China sea basin was a large Cenozoic sedimentary basin, with a thickness of deposition of more than 10 thousand meters.
本文指出东海盆地是一个大型的以新生代沉积为主的盆地，沉积岩厚度超过万米。
This article indicates that east China sea basin was a large Cenozoic sedimentary basin, with a thickness of deposition of more than 10 thousand meters.
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