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- W2363313356 abstract "The synsedimentary tectonic activities and ancient structural frameworks in different evolutionary stages of Chang-chang sag were revealed by the restoration of 3 seismic lines across Chang-chang sag using balanced cross-section technique.On the basis of recognition and redefinition of secondary ancient structural units and its evolutionary types in association with further comprehensive analysis of the controlling of structure evolution on sequence pattern,the sedimentary filling model of Chang-chang sag was established.The results show that the tectonic evolution of Chang-chang sag has experienced three stages,namely the faulted period during Eocene to early Oligocene,the faulted-depressed transition period during late Oligocene and the depression period during Neogene.Correspondingly,there are three superimposed basin prototypes with different structural frameworks in Chang-chang sag.In rifting episodeⅠand rifting episodeⅡ there were mainly updip-basalslope fault abrubt slope belt sequence pattern and step-fault abrubt slope belt sequence pattern,while in rifting episodeⅢ they gradually evolved to downdip-basalslope fault abrupt slope belt sequence pattern and step-fault gentle slope belt sequence pattern.And in the thermal subsidence period there were mainly faulting flexure belt sequence pattern and some downdip-basalslope fault abrubt slope belt sequence pattern,while in the accelerated subsidence period there was only simple flexure belt sequence pattern in Chang-chang sag.The large-scale low stand deltas,low stand fans and incised valley filling relating to fault slope belt and flexure belt should be favorable exploration areas of structural-lithologic reservoir and lithologic reservoir." @default.
- W2363313356 created "2016-06-24" @default.
- W2363313356 creator A5025538834 @default.
- W2363313356 date "2012-01-01" @default.
- W2363313356 modified "2023-09-24" @default.
- W2363313356 title "Tectonic evolution and its controlling on sequence pattern of Chang-chang sag,deepwater area of Qiongdongnan basin,South China Sea" @default.
- W2363313356 hasPublicationYear "2012" @default.
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