层序地层学原理

根据层序地层学原理，松辽盆地下白垩统可划分出五个不整合（T5、T4、T3、T1－1、T03）以及三个层序。

According to the principle of sequence stratigraphy , the Lower Cretaceous could be divided into five unconformities ( T5 , T4 , T3 , T1-1 , T03 ) and three sequences .

应用层序地层学原理，大民屯凹陷古近系可划分为1个二级层序、3个三级层序。

In terms of sequence stratigraphical principles , the Paleogene can be divided into one 2-order sequence and 3-order sequences .

应用层序地层学原理建立沙四段层序格架，划分体系域，明确沙四段沉积体系特征及展布。

Sequence stratigraphy is used to establish s4 sequence frame , divide system tract , and understand s4 sedimentary system and distribution .

在坪北油田沉积微相模型研究中，首先利用高分辨率层序地层学原理进行地层划分对比，建立构造模型；

In the research of the sedimentary microfacies model for Pingbei oilfield , three intermediate cycles are identified by using high-resolution sequence stratigraphy .

应用露头层序地层学原理和方法，首次对滇西古特提斯（昌宁－孟连带）中海山碳酸盐台地的石炭系进行了研究。

Based on the outcrop sequence-stratigraphic principle and method , the authors first studied the Carboniferous section of the seamount carbonate platform in Paleo-Tethys ( the Changning-Menglian belt ), Southwestern Yunnan , China .

同时，在三维地层模型的基础上，根据层序地层学原理，按层序网格表征方式细分地层，建立了层序模型。

At the same time , on the basis of the modeling above and the principles of stratigraphic sequence , following the way of stratigraphic sequence , the stratums are subdivided to get sequence model .

运用层序地层学原理和方法，在黄县盆地进行高频层序地层划分的基础上，对黄县早第三纪断陷盆地充填演化的动力学特征进行研究。

By means of the principle , method and technology of sequence stratigraphy , The dynamic characteristics of filling and evolution of Huangxian Eogene fault basin are studied , based on the classification of high frequency sequences .

依据现代层序地层学原理首次对研究区进行了高分辨率层序地层的划分与对比；

The results and new ideas are as follows : According to the theory of modern sequence stratigraphy , Sha 2 member of the fault block of Tuo 30 were first studied on the division and contrast of high discernible formation sequence .

根据层序地层学原理，分析了高分辨率地震资料的特点，并据此提出了一个地震层序模型，以代替地震褶积模型，用以评价地震分辨率的可靠性。

Based on the principle of sequence stratigraphy , through analyzing the features of high resolution seis - mic data , a seismic sequence model is proposed to substitute the seismic convolution model , so as to evaluate the reliability of seismic resolution .

运用层序地层学原理对该区划分了6个超层序，10个层序，建立石炭系风化面以上到侏罗系层序框架，以及低水位、水进、高水位体系域的平面展布。

By using the principle of sequence stratigraphy , six supersequences and ten sequences are divided in the study area , sequence framework from above Carboniferous weathering surface to Jurassic strata is established , and the plane distribution of lowstand , transgressive and highstand system tracts are determined .

运用高分辨层序地层学的原理和方法，通过基准面旋回对比，建立了高分辨率层序地层格架。

Applying high resolution sequence stratigraphy , the high resolution sequence stratigraphy hack is concluded .

针对陆相地层发育特点，讨论了层序地层学基本原理在陆相地层中应用的可行性。

The author aimed at the character of the continental stratum development to discuss the feasibility of the application of classical sequence stratigraphy to continental stratum .

针对这一问题，首次将层序地层学的原理和方法应用于该区储集砂体分布规律的预测。涡柱构造体微量元素分布规律

The sequence stratigraphy was applied to predict the distribution of sandy reservoirs . STUDY OF THE DISTRIBUTION OF THE TRACE ELEMENTS IN " WHIRLPOOL PILLAR " STRUCTURE

利用P波数据体以层序地层学的方法原理为指导，建立地层和沉积格架；

According to the theory of sequence stratigraphy , we established the stratigraphic and sedimental framework using P-wave seismic database .

本文根据层序地层学的基本原理，对塔里木盆地北部下石炭统沉积体系域的基本特征进行了描述。

Abstract Based on the principles of sequence stratigraphy , the paper described the basic characteristics of depositional system tract in the Lower Carboniferous .

根据层序地层学的基本原理，综合利用露头、钻井、测井和地震等资料，建立汤原断陷古近系层序地层格架，识别出2个超层序、11个三级层序。

The sequence framework of Tangyuan fault depression is divided into 2 supersequence sets and 11 third-order sequences in Paleocene according to the theory of sequence stratigraphy , natural outcrop , and data of drilling , logging and seism .

运用层序地层学的方法原理，进行单井和联井高分辨率层序地层对比，结合测井相、地震相研究确定沉积特征，并运用地震岩性反演技术，搞清砂体的叠置关系和横向分布特征。

We do high resolution sequence stratigraphy contrast of single well and well tip using the sequence stratigraphy principle , confirm sedimentary characters by logging facies and seismic facies , recognize superimposed relationship and transverse distributing of sand body by seismic-lithology inversion .