Controls of accommodation to sediment-supply ratio on sedimentary architecture of continental fluvial successions  

作　　者：Wei Li Da-Li Yue Yu-Shan Du Jian Li Chi Zhang Zhi-Qiang Gong Xue-Ting Zhang Qing-Lin Shu Jian Gao 

机构地区：[1]National Key Laboratory of Petroleum Resources and Engineering,China University of Petroleum(Beijing),Beijing,102249,China [2]College of Geosciences,China University of Petroleum(Beijing),Beijing,102249,China [3]Shengli Oil Field Company,SINOPEC,Dongying,Shandong,257015,China [4]PetroChina Research Institute of Petroleum Exploration&Development,Beijing,100083,China

出　　处：《Petroleum Science》2023年第4期1961-1977,共17页石油科学(英文版)

基　　金：This research was financially supported by the National Natural Science Foundation Project of China(No.42202109,42272186);the China Postdoctoral Science Foundation1(BX20220351,2022M713458);the Research Institute of Petroleum Exploration and Development,China(2021DJ1101);the Cooperation Project of the PetroChina Corporation(ZLZX2020-02);Anonymous reviewers are thanked for their constructive comments,which helped improve the paper.Additionally,associate professor Luca Colombera is thanked for his suggestions and language polishing work.

摘　　要：The applicability of sequence stratigraphic models to continental fluvial successions has long been topic for debate. To improve our understanding of how fluvial architectures record responses to changes in the ratio between accommodation rate and sediment-supply rate (A/S), two case studies are analyzed, including a densely drilled subsurface fluvial reservoir imaged with a seismic cube, and an outcropping fluvial succession. The subsurface dataset provides a larger, three-dimensional perspective, whereas the outcrop dataset enables observation at higher resolution. On the basis of both datasets, channel-body density, channel-body stacking patterns and their formative river types are interpreted at different scales, and how these may reflect responses to A/S change (the rate of accommodation creation relative to the rate of sediment supply) are discussed. The results indicate that (i) channel-body stacking patterns undergo four evolutionary stages along with the A/S increase, i.e., multi-story, mixed multi- and two-story, two-story, and isolated patterns;(ii) channel-body density decreases along with the channel-body stacking patterns varying from multi-story to isolated;(iii) formative rivers types are interpreted as evolving from braided planforms to braided-meandering planforms and then to meandering ones, with the increase of A/S.

关 键 词：Channel body Sedimentary architecture Stacking pattern Formative river type Sequence stratigraphy A/S 

分 类 号：P512.2[天文地球—地质学] P343.5