构造活动是控制沉积盆地形成的主要因素。
Structure is the main factor which controls the sedimentary basin formation.
黔南泥盆纪沉积盆地是一个停滞缺氧盆地。
The sedimentary basin of Devonian in Southern Guizhou, South China is euxinic.
压实作用与沉积盆地发育的整个过程有关。
Stratigraphic compaction is related to the evolutionary process of the basin.
陆良盆地是云南第三系沉积盆地的典型代表。
Luliang basin is a typical representative of the Tertiary sedimentary basins in Yunnan Province.
陆良盆地是云南省第三系沉积盆地的典型代表。
Luliang basin is a typical representative of Tertiary sedimentary basins in Yunnan Province.
陆良盆地是云南省第三系沉积盆地的典型代表。
Luliang basin is a typical one of the Tertiary sedimentary basins in Yunnan Province.
四合屯地区位于一个中生代火山沉积盆地之中。
Sihetun area is situated in a Mesozoic volcanic-sedimentary basin.
并简要分析了中国沉积盆地特殊的油气赋存特征。
Finally, the unusual characteristics of oil and gas distribution in Chinese sedimentary basins are briefly discussed.
粤北晚古生代沉积盆地存在三种类型的矿化流体。
There are three types of mineralization fluid in Later Paleozoic sedimentary basin in North-Guangdong province.
磷灰石裂变径迹是研究沉积盆地地热史的强有力工具。
Apatite fission track is a powerful tool to study the thermal history of sedimentary basin.
研究主要集中在各种类型的沉积盆地的构造和形成机制。
Research focuses on various types of sedimentary basins and their tectonic mechanisms of formation.
在超压沉积盆地中，超压传递可能是一种较普遍的现象。
Overpressure transference may be a kind of widespread phenomenon in overpressure sedimentary basins.
在许多沉积盆地中，地层水的含盐量随深度或压实作用而增高。
In many sedimentary basins the salinity of the formation water increases with depth or compaction.
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.
西南小盆地为单层结构箕状断陷型和双层（地）台、断（陷）型沉积盆地。
The small basin in the southwest of China is types of single structure halfgraben-like depression and dual structures platform-fault depression.
在沉积盆地中，碳氢化合物很常见，而在间杂的火成岩与变质岩中则找不到。
Hydrocarbons commonly occur in sedimentary basins and are absent from intervening areas of igneous and metamorphic rocks.
柞山地区为一泥盆纪热水沉积盆地，其遥感环形构造是矿化集中区的基本格局。
Zhashan area is a slurry sedimentary basin, it's remote annular structure is main pattern of mineral region.
最后，作者展望了层序地层学在陆相沉积盆地内砂岩型铀矿找矿中的应用前景。
Finally, the authors look ahead the application potential of sequence stratigraphy to the prospecting for sandstone type uranium deposits in continental depositional basins.
根据盆地形成演化历史及结构特征，将中国沉积盆地划分为单型与叠合型两大类。
According to basin's evolutional history and structural features, the sedimentary basins in China can be divided into monotype and superimposed type basins.
随着陆相沉积盆地研究中层序地层学的引入，在国内引起了一些颇有争议的问题。
With the introduction of Sequence Stratigraphy into the study of continental sedimentary basins, some controversial questions arose in our country.
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.
利用流体包裹体热动力学模拟技术获取沉积盆地古压力已广泛用于石油勘探领域。
The acquisition of paleopressure using the thermodynamic simulation technology of fluid inclusion has been widely used in the field of petroleum exploration.
南海是东亚古季风产物的主要沉积盆地，保存着比陆地更加完整和连续的沉积记录。
The South China Sea is the major deposit basin of the East Asian paleomon-soon products, and is preserving more integrated and continuous deposit record thanland.
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.
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.
例如，航磁图除可以展示出一个沉积盆地的总体趋势和走向，也可揭露大量的细节部分。
For example, airborne, magnetic maps shows a lot of general trends in a sedimentary basin, and usually a lot of details too.
随着地浸技术的引进与不断完善，沉积盆地砂岩型铀矿床已经成为我国铀资源找矿重点。
As the development of in-situ leaching technique, sandstone-type uranium deposits have become the key prospecting target for uranium resources in China.
并对组成喜马拉雅造山带各种主要沉积盆地进行了构造沉降分析，研究盆地演化动力机制；
The tectonic subsidence analysis and dynamic mechanism of the basin evolution are processed in the main sedimentary basins across this belt.
并对组成喜马拉雅造山带各种主要沉积盆地进行了构造沉降分析，研究盆地演化动力机制；
The tectonic subsidence analysis and dynamic mechanism of the basin evolution are processed in the main sedimentary basins across this belt.
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