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地层学的研究是以地层单位的物质形式运作的。The study of stratigraphy is playing in the form of units.

地层学研究地壳中岩石的层序。Stratigraphy studies the sequence of the rocks in the earth's crust.

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牙形石是一类在地层学研究中具有重要意义的古生物化石。Conodont is an important kind of fossil in the stratigraphy research.

他们的主要精力放在研究天然露头的地层情况与构造上。Their main effort is directed to stratigraphy and structure of outcrops.

层序地层学原理可以应用于湖相沉积。The principle of sequence stratigraphy can be used in lacustrine deposit.

晚第四纪古河口湾的发育及有关的资源环境问题。Late Quaternary stratigraphy and evolution of the Changjiang Delta, China.

地层学是地质学的一门重要的基础学科。Stratigraphy is one of the basic subjects of most significance in geology.

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生物地层学是地层学中最基本的也是应用最广泛的一个分支学科。Biostratigraphy is one of the basic and widely applied branches in stratigraphy.

古生物学和地史学及地层学是地质学的不同分支学科。Palaeontology , historical geology and stratigraphy are different subjects of geology.

沉积基准面旋回变化控制着陆相层序地层的形成与演化。Depositional base-level cycle controls the development and evolution of sequence stratigraphy.

陆相含油气盆地中层序地层学的研究不同于海相盆地。Research of sequence stratigraphy in nonmarine petroliferous basin must introduce some new concepts.

这种自我研究使他成为了解剖学和地质学之父。The consequences of this self-study is that he is considered the father of geology and stratigraphy.

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沉积基准面旋回变化控制着陆相层序地层的形成与演化。Changes in depositional base-level cycle control the development and evolution of sequence stratigraphy.

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.

矿床成因属风化残积型，受地层、岩性的控制。Genetically, it is an eluvial deposit produced by weathering, controlled by the stratigraphy and lithology.

地震地层学是按照地震资料解释进行地层学和沉积相的研究。Seismic stratigraphy is the study of stratigraphy and depositional facies as interpreted from seismic data.

高分辨率层序地层学克服了岩性地层对比穿时的缺点。High-resolution sequence stratigraphy overcomes the fault of diachroneity in lithostratigraphic correlation.

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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。Now sequence stratigraphy is widely accepted, and is becoming standard technology of stratigraphical research.

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。Stratigraphy traps can be classified into stratigraphic onlap trap and stratigraphic erosion unconformity trap.

传统的层序地层学解释方法只是仅仅使用了常规的地震剖面和测井曲线。Conventional sequence stratigraphy interpreting methods are only using convention seismic and well -logging data.