作者:Yu-xi Zhang,Jian-wen Chen,Jiang-yu Zhou,Yong Yuan
摘要:Based on well logging and seismic data, combined with a comparative analysis of drilling data in the Lower Yangtze region, the sequence stratigraphic framework of the Qinglong Formation was established and divided into four third-order sequences. Each sequence is mainly composed of the transgress system tract (TST) and the high-stand system tract (HST). According to the lithology, logging curve and seismic reflection structure, the sedimentary filling characteristics and evolution law for the sequence are analyzed. The results show that each sequence is dominated by a half-cycle decline of sea level, and the rise-fall of sea level controls the distribution and evolution of sedimentary systems within the sequence. During the relative sea-level rise, sedimentation rates slow down and muddy sediments are developed. The characteristics of condensing intervals on the flooding surface are very obvious, and continental shelf and open platform deposition are mainly developed. During the relative decline of sea level, the thickness of sediments increased. The main developments were restricted platform and platform shoal environment, and locally developed evaporation platform environment.
发文机构:Faculty of Earth Resource Qingdao Institute of Marine Geology
关键词:LowerTRIASSICSequenceSTRATIGRAPHYSEA-LEVELchangeCarbonaterocksMarineGEOLOGICALsurveyengineeringYellowSeaChina
分类号: P[天文地球]