对黄河口凹陷新近系进行构造单元划分，分析了凹陷不同层位构造特征异同。
The tectonic units are divided as well as the similarities and differences of structural characteristic are compared in Neogene.
马朗凹陷是三塘湖盆地的一个二级构造带，侏罗系是盆地内主要含油层位。
Malang Depression is a secondary structural belt of Santanghu basin, Jurassic Series is the main oil and gas reservoir of the basin.
本文通过对六苴铜矿床的矿床地质特征分析，认为控矿因素可归结为下列几个方面：层位、岩性、构造、岩相、古地理等。
According to the geological characteristics of Liuju copper deposits, the controlling ore-forming factors include stratigraphy, lithology, structure, lithofacies and paleogeography.
在相同构造背景下，山旺盆地、包家河盆地和青山盆地的中新世对应层位的层序发育特征具有可比性。
With the same geological structural Settings, the Miocene sequence development of the Shanwang, Baojiahe, and Qingshan Basins are comparable.
金矿化受层位、构造、蚀变控制明显。
Gold mineralization is evidently controlled by stratigraphic horizon, structures and alteration.
地震层位标定是地震资料构造解释和地震储层研究的基础。
Seismic horizons labeling is basis of structural interpretation of seismic data and study of seismic reservoir.
喀什凹陷北部地表构造出露有多处油砂，分布层位主要是中新统安居安组和帕卡布拉克组，次为下白垩统克孜勒苏群。
Oilsand has been found in many ground structures in northern Kashi sag, which distributed mainly in Miocene Anjuan andPakabulake Formation, secondly in Lower Cretaceous Kzlesu Formation.
结论对于构造变动强烈、烃源岩层位多、热演化历程复杂的叠合盆地，其油气藏类型复杂，油气勘探的难度增大。
Conclusion the types of reservoir are complex, and the exploration of petroleum is every difficult in the basin of strong structural movement, multi-layer source rocks, complex thermal history.
而岩溶分布的层位及构造部位，在同一地质单元中的浅层和深层区具有类似性。
In the same geological formation, the similarity in distribution is observed for both shallow and deep layers.
在利用地震层位构造图编制盆地区域性等厚图时，可以用断层面的残留厚度来描绘断层在平面上的分布。
In compiling areal isopach of a basin from seismic horizon structure map, we can use the residual thickness at both sides of fault plane to show the horizontal distribution of a fault.
针对算法缺点提出了手动拾取反射层位的思想以改进该算法，利用手动拾取层位的思想极大的减弱了构造项的影响。
In order to resolve the shortcomings of the algorithm, this paper proposes the idea that it picks up the reflections time layer by artificial and it can weaken the impact of structural items.
该矿床地质工作及研究程度极低，铜钴矿体明显受万保沟群基性火山岩层位及断裂构造控制。
The degree of geological work and research for the deposit is quite low. The ore body is obviously controlled by basic igneous rocks of Wanbaogou group and structural faults.
该矿床地质工作及研究程度极低，铜钴矿体明显受万保沟群基性火山岩层位及断裂构造控制。
The degree of geological work and research for the deposit is quite low. The ore body is obviously controlled by basic igneous rocks of Wanbaogou group and structural faults.
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