高位体系域表现为加积—进积沉积特征。
Highstand system tracts are characterized by acceleration progradation sedimentation.
高位体系域为厚层块状岩盐夹薄层泥岩和砂岩。
Highstand system tracts are formed by thick-massive rock salts intercalated by thin layers of mudstone and sandstone.
高位体系域主要发育滨浅湖相、河流相及进积型三角洲沉积体系。
Highstand System Tract mainly develops depositional system of offshore-meare, fluvial facies and prograded delta.
早、中侏罗世低位体系域不发育，由海进体系域与高位体系域两部分组成。
Lowstand System Tracts of Early and Metaphse Jurassic Period was undergrown, of which Transgressive Systems Tract and Highstand Systems Tract made up.
碳酸盐岩烃源岩的形成是受层序体系域和沉积相控制，分布于下斜坡的高位体系域或与膏盐岩伴生。
The carbonate source rock is controlled by system tracts and facies. The carbonate source rock is mainly developed in high system tract in low ramp or is survived with gypsum-salt rock together.
各层序分别由低位体系域的下切谷充填沉积的砂岩、砂砾岩，海侵体系的灰岩、泥灰岩、泥岩、煤和高位体系域的碎屑岩和煤组成。
Each sequence is composed of incised valley sandstone of low system tract, limestone, marl, coal and mudstone of transgressive system tract and clastics and coal of high system tract.
层序S2是一个三分层序，包含低位、湖侵和高位三个体系域。进一步可以划分为3个准层序组和12个准层序。
The S2 sequence is a tripartition dichotomize sequence , include the LST , TST and HST, further divided 3 parasequence formations and 12 parasequence.
层序S2是一个三分层序，包含低位、湖侵和高位三个体系域。进一步可以划分为3个准层序组和12个准层序。
The S2 sequence is a tripartition dichotomize sequence , include the LST , TST and HST, further divided 3 parasequence formations and 12 parasequence.
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