Stratigraphy is used for dating portable art.
地层学被用于测定可移动艺术品的年代。
The study of stratigraphy is playing in the form of units.
地层学的研究是以地层单位的物质形式运作的。
The mineralization is mainly controlled by stratigraphy and structures.
矿化主要受地层和构造的控制。
From the view of stratigraphy, they all belong to the Cretaceous period.
从地层学上看，它们都属于白垩纪。
Sequences are the fundamental unit of interpretation in sequence stratigraphy.
层序是层序地层学解译的基本单位。
High resolution sequence stratigraphy has become an important way for oil exploration.
高精度层序地层学研究已成为进行油气勘探的重要手段之一。
The second dating method was palaeo - magnetic analysis, or magnetic polarity stratigraphy .
第二种测定法是古磁学分析法，也叫磁极地层学测定法。
Kongnan Area; Shahejie Period; Sequence Stratigraphy; Tectonic - Sedimentary Response Model.
孔南地区；沙河街期；层序地层；构造-沉积响应模型。
Depositional base-level cycle controls the development and evolution of sequence stratigraphy.
沉积基准面旋回变化控制着陆相层序地层的形成与演化。
Research of sequence stratigraphy in nonmarine petroliferous basin must introduce some new concepts.
陆相含油气盆地中层序地层学的研究不同于海相盆地。
The exploration proved that the study of stratigraphy sequence and sedimentary system is the key tache.
勘探实践证明，层序地层与沉积体系研究是隐蔽油气藏勘探的关键基础性环节。
Coal geology emphatically studies always stratigraphy and sedimentology of coal and coal-bearing strata.
煤地质学一直偏重于对煤和含煤地层的地层学和沉积学的研究。
Coal geology emphatically studies always stratigraphy and sedimentology of coal and coal bearing strata.
煤地质学一直偏重于对煤和含煤地层的地层学和沉积学的研究。
Changes in depositional base-level cycle control the development and evolution of sequence stratigraphy.
沉积基准面旋回变化控制着陆相层序地层的形成与演化。
The aim of the study was undertaken to better characterise and map the shallow stratigraphy and structure.
此研究的目的是进一步弄清浅地层的结构，并绘制图形。
Now sequence stratigraphy is widely accepted, and is becoming standard technology of stratigraphical research.
层序地层学现在得到广泛承认，已经成为研究地层的标准技术。
Stratigraphy traps can be classified into stratigraphic onlap trap and stratigraphic erosion unconformity trap.
地层圈闭可分为地层超覆不整合圈闭和地层削蚀不整合圈闭。
It is practically proved that the key exploration technologies are reservoir prediction and sequence stratigraphy.
实践表明，该领域勘探研究的核心技术是地震储集层预测与层序地层学。
The contrast of high-resolution sequence stratigraphy is one of the effective ways of high-resolution isochronic correlation.
高分辨率层序地层对比是高分辨等时对比的一种有效方法。
This paper introduces the derivation and basic concept of the non Smith stratigraphy and the present development in its research.
简要地叙述了“非史密斯地层学”术语的由来、基本概念及研究近况。
With study on biological stratigraphy, geochron stratigraphy, and lithologic stratigraphy, Permian is re-divided in Sichuan Basin.
通过生物地层、年代地层、岩石地层的研究，对四川盆地二叠系进行重新划分。
The type of parasequence sets is similar to classic sequence stratigraphy, and the parasequence mainly consists of positive rhythm.
准层序组类型与经典层序地层学中的类型相似，但是其内部各准层序以正韵律为主。
On one hand, new experimental technologies are used continuously to explore the metallogenic mechanism of stratigraphy, structure etc.
一方面，人们将继续采用新的实验技术去了解地层、构造等因素的控矿机理。
By using the analytical method of sequence stratigraphy and sediment system, an isochronous unit of Biyang Depression was established.
应用层序地层学和沉积体系分析方法，建立了泌阳凹陷的等时地层单元。
Sedimentary facies study integrating drilling, log and seismic data and using sequence stratigraphy is a base of petroleum exploration.
综合钻井、测井和地震资料，用层序地层学方法进行沉积相研究是油气勘探的基础。
On the one hand, new experimental technologies are used continuously to explore the metallogenic mechanism of stratigraphy, structure etc.
一方面，人们将继续采用新的实验技术去了解地层、构造等因素的控矿机理。
High resolution sequence stratigraphy of Cangfanggon Group in Jimusa'er Area is studied based on a microfacies analysis of surface outcrop.
在对地表露头的微相分析基础上，对吉木萨尔地区仓房沟群进行高分辨率层序地层学研究。
Through sequence stratigraphy, widely-separated sediments that occur between correlatable unconformities could be compared with each other.
通过层序地层学研究，产生于可对比不整合广泛分离的沉积物可以彼此比较。
Carbonate reservoirs can be divided into intra-sequence reservoirs and sequence boundary reservoirs based on study of sequence stratigraphy.
利用层序地层学研究可将碳酸盐岩储层分为层序内部储层和层序界面储层。
Carbonate reservoirs can be divided into intra-sequence reservoirs and sequence boundary reservoirs based on study of sequence stratigraphy.
利用层序地层学研究可将碳酸盐岩储层分为层序内部储层和层序界面储层。
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