海洋地质前沿2026，Vol.42Issue(9)：44-56,13.DOI:10.16028/j.1009-2722.2025.183
四川盆地威远地区奥陶系宝塔组海相碳酸盐岩沉积特征及模式
Sedimentary characteristics and sedimentary model of marine carbonate rocks of the Ordovician Baota Formation in Weiyuan area,Sichuan Basin
摘要
Abstract
The Upper Ordovician Baota Formation is a new and emerging hot spot for carbonate petroleum ex-ploration in the Sichuan Basin,SW China.For a long time,there have been insufficient studies on the deposition-al environment of the Baota Formation in the Weiyuan area,which has restricted the progress of petroleum explor-ation and development in this area and the understanding of the Ordovician paleogeographic pattern in the Sichuan Basin.By integrating outcrop analysis,drilling,logging,seismic,and thin section data,we clarified the sediment-ary facies types and distribution patterns of the Baota Formation in the Weiyuan area,and revealed that the paleo-topographic scheme of"high in the NW and low in the SE"was governed by the Central Sichuan Paleouplift in the sedimentary evolution of the Baota Formation.Results show that the sedimentary environment of the Baota Formation in the Weiyuan area is significantly different from those in the southern and eastern(northern)areas of Sichuan Province.Three main sedimentary facies types,i.e,dolomitic platform(dolomite flat),tidal flat-associ-ated reef-shoal complex,and restricted platform,were recognized.The dolomitic platform facies is mainly fine to medium crystalline dolomite.The tidal flat-reef-shoal complex facies is thick-bedded limestone,in which a partial dolomitization belt was developed in windward high terrain area of reef-shoal body,with dolomitic limestone and(partially)dolomitized limestone developed.The restricted platform facies is mainly interbedded micritic and grainy limestone,with common horizontal bedding and bioturbation structures and typical desiccation cracks,in-dicating restricted water circulation.Through the analysis of the vertical evolution and lateral comparison of sedi-mentary facies,we believe that the sedimentary scheme of the Baota Formation in the Weiyuan area transitioned southeastward from dolomitic platform and tidal flat-reef-shoal complex to restricted platform.The dolomite of the dolomitic platform facies and the partial dolomitization zone on the windward side of the tidal flat-reef-shoal complex facies are favorable reservoirs(prospective reservoir intervals).This study deepened our understanding of the Ordovician paleogeography in the Sichuan Basin and provided a new theoretical basis for reservoir predic-tion in this area.关键词
宝塔组/碳酸盐岩/沉积相/威远地区/四川盆地Key words
Baota Formation/carbonate rock/sedimentary facies/Weiyuan area/Sichuan Basin分类
海洋科学引用本文复制引用
卢嘉勋,邓雅霓,严雪齐,苟哲培,向柯函,杜彦熹,崔智斌,谭先锋,刘田,耿超,魏倩倩,胡浩,沈秋媛,杨坚,崔玉娜,李成海..四川盆地威远地区奥陶系宝塔组海相碳酸盐岩沉积特征及模式[J].海洋地质前沿,2026,42(9):44-56,13.基金项目
国家自然科学基金(42572138) （42572138）
重庆市杰出青年科学基金(CSTB2025NSCQ-JQYXZZXMX0001) （CSTB2025NSCQ-JQYXZZXMX0001）
