Application of balanced section technique to the study of positive inversion structure and hydrocarbon accumulation control in Xihu Depression of East China Sea
LI Rui-sheng, Moe Key
Abstract
LI Rui-sheng, Moe Key
Abstract
Balanced section technique has been applied to the study of the stage and strength of the Tertiary positive inversion structure in Xihu Depression of East China Sea. The Xihu Depression is recognized as a 3-stage inversion of early, medium and late inversion. The early inversion in late Eocene mainly occurred in the western slope of the basin, and the inversion strength increased from south to north in the study area. The medium reversion in late Oligocene mainly occurred in the eastern fault zone of the basin, and the inversion strength decreased from south to north in the study area. The late inversion in late middle-Miocene mainly occurred in the central uplift belt of the basin, and the inversion strength increased from south to north in the study area. The inversion action generally intensified along time. The inversion action had formed various structural traps which were large and intact, and very favorable to oil and gas migration and accumulation. Meanwhile, the inversion action also had a transformation effect on reservoir physical property. Present exploration shows that the three structural inversion belts are most favorable zones for oil and gas prospecting in Xihu Depression.
OpenAlex reports 5 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Balanced section technique has been applied to the study of the stage and strength of the Tertiary positive inversion structure in Xihu Depression of East China Sea. The Xihu Depression is recognized as a 3-stage inversion of early, medium and late inversion. The early inversion in late Eocene mainly occurred in the western slope of the basin, and the inversion strength increased from south to north in the study area. The medium reversion in late Oligocene mainly occurred in the eastern fault zone of the basin, and the inversion strength decreased from south to north in the study area. The late inversion in late middle-Miocene mainly occurred in the central uplift belt of the basin, and the inversion strength increased from south to north in the study area. The inversion action generally intensified along time. The inversion action had formed various structural traps which were large and intact, and very favorable to oil and gas migration and accumulation. Meanwhile, the inversion action also had a transformation effect on reservoir physical property. Present exploration shows that the three structural inversion belts are most favorable zones for oil and gas prospecting in Xihu Depression.
Key concepts: Inversion (geology), Geology, Structural basin, Prospecting, China sea, Seismology, Paleontology, Oceanography