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facies sequence
    STUDY ON ALLUVIAL-FLUVIAL FACIES SEQUENCE STRATIGRAPHY
    冲积-河流相层序地层学研究
    Discussion on the stratigraphic model in alluvial-fluvial facies sequence and its application in Jiyang depression.
    冲积—河流相层序地层模式探讨及其在济阳坳陷的应用
    Study on Alluvial-Fluvial Facies Sequence Stratigraphy and Favorable Reseivoir Zones Prediction for Neogene, Inshore Area, Jiyang Depression
    济阳坳陷滩海地区新近系冲积-河流相层序地层研究与有利成藏区带预测
    The Distribution of Sedimentary Organic Facies in the Continental Facies Sequence Stratigraphic Framework: an example from Middle Jurassic coal bearing series in the Taibei sag of the Turpan Hami basin and Southern Junggar basin
    沉积有机相在陆相层序地层格架中的分布特征——以吐哈盆地台北凹陷及准噶尔盆地南缘中侏罗世煤系为例
    Fluvial Facies Sequence Stratigraphy Discuss
    河流相层序地层学研究
    The primary control factors of fluvial facies sequence forming are structure factor or palaeotopography, climate factor and sediment supply. It is possible that palaeotopography and climate factors influence fluvial facies sequence forming and development macrofeature more apparently.
    河流相层序形成的主控因素为构造因素(或古地形)、气候因素和沉积物补给,而古地形和气候因素对冲积—河流相层序形成与发育宏观特征的影响可能更为明显,在河流相层序地层分析中,基准面,而不是海(湖)平面是层序研究的主要参照面。
    This article also summarizes facies mark, facies sequence, facies model and sandbody spreading character of lowstand delta.
    低位三角洲发育在主要物源区的前方 ,处在深湖相泥岩包围之中 ,相标志、相层序、相模式和砂体的展布特征有别于深水重力流沉积 ,是重要的油气储集体。 图 4参 18
    Based on the log response of different sedimentary microfacies, the distribution character of the sedimentary facies in the plane is researched, and the facies sequence and pattern of this area are summed up.
    根据不同沉积微相的测井响应特征,研究了沉积相在平面上的分布特征,并总结出研究区的相层序和相模式。
    Based on sequence division and stratigraphic correlation, sedimentary features of lacustrine facies sequence and fluvial facies sequence are analyzed, and a sequence stratigraphic model is built in the study area.
    在此基础上,分析了湖泊相和河流相层序的沉积特征,总结了本区层序地层的发育模式。
 

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