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。
Sedimentary facies study integrating drilling, log and seismic data and using sequence stratigraphy is a base of petroleum exploration.
采取点、线、面相结合， 岩石地层学、 生物地层学和同位素年代学相结合的工作方法，研究了这套地层的层序、划分和对比问题；
The succession, division and correlation of these strata are studied with lithostratigraphy, biostratigraphy and isotopic geochronology methods and by the combination of of point, line and area.
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.
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。
By using the analytical method of sequence stratigraphy and sediment system, an isochronous unit of Biyang Depression was established.
运用钻井岩心及层序地层学有关理论、方法，对木里煤田聚乎更矿区中侏罗统含煤岩系进行了层序地层学研究。
The sequence stratigraphy of the Middle Jurassic coal-bearing measures in the Juhugeng mine area in Qinghai Province was studied by using the core and logging data.
应用层序地层学和地震岩性反演相结合的方法对东濮凹陷胡状集地区有利的储层发育区进行了预测。
Sequence stratigraphy and seismic lithologic inversion were used to predict favourable reservoir developed area in Huzhuangji Region, Dongpu Depression.
运用露头层序地层学原理及沉积体系分析方法，对随州盆地晚白垩世“红层”进行了层序地层学的研究。
Applying sequence stratigraphy principle and sedimentary system analysis, the "red beds" in Upper Cretaceous Epoch in Suizhou basin has been studied on sequence stratigraphy.
“九五”期间四川西康群区区调的实践也证明，在造山带复理石区填图中，海底扇法是一种比层序地层学更可行、更有效、更直观的方法。
The practical application of this method in the orogenic belt in the western Sichuan has been proved to be feasible and effective.
今后的研究方向是不同地区不同沉积体系的岩性地层圈闭的勘探方法、圈闭与层序地层学的关系、岩性圈闭的地球物理检测技术与综合地质因素的结合等。
The further study lies in the exploration means of different traps, the relations of the traps to sequence stratigraphy, and combination of geophysical technology with synthesizing the geofactor.
层序地层学为沉积盆地分析的一个重要手段和方法。层序地层学在沉积盆地分析中的参数包括宏观参数和微观参数。
As an important method, the parameter of sequence stratigraphy applied to the sedimentary basin includes macroscopic one and microcosmic one.
在凝缩体的概念、陆相盆地中湖相沉积层序形成的主控因素、体系域的划分以及陆相层序地层学的研究方法等方面，提出了探讨性的意见。
The concept of condensed body, main controlling factors of lacustrine sedimentary sequence, classification of system tracts, and research methods of continental sequence stratigraphy are discussed.
在凝缩体的概念、陆相盆地中湖相沉积层序形成的主控因素、体系域的划分以及陆相层序地层学的研究方法等方面，提出了探讨性的意见。
The concept of condensed body, main controlling factors of lacustrine sedimentary sequence, classification of system tracts, and research methods of continental sequence stratigraphy are discussed.
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