Through precisely measured data of field outcrops,wells logging data and samples analytical data in the research area,it is considered that the topography of the sedimentary period of Xiaoheba formation is relatively ...Through precisely measured data of field outcrops,wells logging data and samples analytical data in the research area,it is considered that the topography of the sedimentary period of Xiaoheba formation is relatively flat,the water flow is shallow and wide and the fluctuation is frequent,the supply of source is abundant,and it has favorable sedimentary conditions to forming shallow-river fluvial-dominated delta.The delta in the research area is a distal-basin sedimentary,and due to multiple branches and long extension of the river channel,there are large area of delta front sand deposits with fine grained development,high maturity and underwater environment existed within the research area.The Xiaoheba formation in the Jiannan-Fuling three-dimensional seismic region has the obvious characteristics of strong peak progradation reflection.Based on the above analysis,the sedimentary mode of shallow-river fluvial-dominated delta of Xiaoheba formation of Southeastern Sichuan Basin is established and the reservoir forming conditions are discussed.It is considered that the Xiaoheba formation has excellent hydrocarbon source,high-quality reservoirs and effective migration channel.This research has certain guiding significance for the next stage of tight marine clastic rocks oil and gas exploration of Southeastern Sichuan Basin.展开更多
The distinctive characteristics of the modern Pearl River delta formation and development are divided phases, diversity and imbalance in spatial and temporal. The delta was moving seaward gradually in a long period af...The distinctive characteristics of the modern Pearl River delta formation and development are divided phases, diversity and imbalance in spatial and temporal. The delta was moving seaward gradually in a long period after the last Holocene glacial stage and the ancient drowned Pearl River estuary was predominated by tide. The delta was expanding quickly since fluvial force was turned to be leading status about 2500 years ago. The sediment grain size was changing longitudinally from coarser to finer. As well as the finer sediment may be reworked and redistributed shoreward by tidal current nearby the river mouth. And the fluvial-dominated delta is developed by the mutual deposition reflected in the vertical direction. According to the spatial difference of land-ocean interaction, the main body of the Pearl River delta which is the fluvial-dominated and protruding seaward is coupled with or concomitant with the estuaries and tide-dominated deltas which are adjoined to both sides of the main part like two展开更多
基金Funded by National Science and Technology Major Project of China(No.2016ZX05002004-004).
文摘Through precisely measured data of field outcrops,wells logging data and samples analytical data in the research area,it is considered that the topography of the sedimentary period of Xiaoheba formation is relatively flat,the water flow is shallow and wide and the fluctuation is frequent,the supply of source is abundant,and it has favorable sedimentary conditions to forming shallow-river fluvial-dominated delta.The delta in the research area is a distal-basin sedimentary,and due to multiple branches and long extension of the river channel,there are large area of delta front sand deposits with fine grained development,high maturity and underwater environment existed within the research area.The Xiaoheba formation in the Jiannan-Fuling three-dimensional seismic region has the obvious characteristics of strong peak progradation reflection.Based on the above analysis,the sedimentary mode of shallow-river fluvial-dominated delta of Xiaoheba formation of Southeastern Sichuan Basin is established and the reservoir forming conditions are discussed.It is considered that the Xiaoheba formation has excellent hydrocarbon source,high-quality reservoirs and effective migration channel.This research has certain guiding significance for the next stage of tight marine clastic rocks oil and gas exploration of Southeastern Sichuan Basin.
基金This work was supported by the National Natural Science Foundation of China (Grant No. 49776304).
文摘The distinctive characteristics of the modern Pearl River delta formation and development are divided phases, diversity and imbalance in spatial and temporal. The delta was moving seaward gradually in a long period after the last Holocene glacial stage and the ancient drowned Pearl River estuary was predominated by tide. The delta was expanding quickly since fluvial force was turned to be leading status about 2500 years ago. The sediment grain size was changing longitudinally from coarser to finer. As well as the finer sediment may be reworked and redistributed shoreward by tidal current nearby the river mouth. And the fluvial-dominated delta is developed by the mutual deposition reflected in the vertical direction. According to the spatial difference of land-ocean interaction, the main body of the Pearl River delta which is the fluvial-dominated and protruding seaward is coupled with or concomitant with the estuaries and tide-dominated deltas which are adjoined to both sides of the main part like two
