A unique lacustrine mixed dolomitic-clastic sequence for tight oil reservoir within the middle Permian Lucaogou Formation of the Junggar Basin, NW China: Reservoir characteristics and origin

• Published in: Marine and petroleum geology 2016-09, Vol.76, p.115-132
• Main Authors: Wu, Haiguang, Hu, Wenxuan, Cao, Jian, Wang, Xiaolin, Wang, Xulong, Liao, Zhiwei
• Format: Article
• Language: English
• Subjects: Basins; Dolomite; Formations; Freshwater; Hydrocarbon fluid; Junggar Basin; Marine; Middle Permian Lucaogou Formation; Mixed dolomites and clastics; Origins; Reservoirs; Rocks; Scanning electron microscopy; Secondary pores; Siltstone; Tight oil reservoir
• ISSN: 0264-8172; 1873-4073
• DOI: 10.1016/j.marpetgeo.2016.05.007

The middle Permian Lucaogou Formation in the Jimusaer Sag of the southeastern Junggar Basin, NW China, was the site of a recent discovery of a giant tight oil reservoir. This reservoir is unusual as it is hosted by lacustrine mixed dolomitic-clastic rocks, significantly differing from other tight reservoirs that are generally hosted by marine/lacustrine siliciclastic–calcitic sequences. Here, we improve our understanding of this relatively new type of tight oil reservoir by presenting the results of a preliminarily investigation into the basic characteristics and origin of this reservoir using field, petrological, geophysical (including seismic and logging), and geochemical data. Field and well core observations indicate that the Lucaogou Formation is a sequence of mixed carbonate (mainly dolomites) and terrigenous clastic (mainly feldspars) sediments that were deposited in a highly saline environment. The formation is divided into upper and lower cycles based on lithological variations between coarse- and fine-grained rocks; in particular, dolomites and siltstones are interbedded with organic-rich mudstones in the lower part of each cycle, whereas the upper part of each cycle contains few dolomites and siltstones. Tight oil accumulations are generally present in the lower part of each cycle, and dolomites and dolomite-bearing rocks are the main reservoir rocks in these cycles, including sandy dolomite, dolarenite, dolomicrite, and a few dolomitic siltstones. Optical microscope, back scattered electron, and scanning electron microscope imaging indicate that the main oil reservoir spaces are secondary pores that were generated by the dissolution of clastics and dolomite by highly acidic and corrosive hydrocarbon-related fluids. •A unique tight oil-hosted lacustrine dolomitic-clastic mixed sequence was described.•Petrologic and δ13C and δ18O signatures were used to characterize this sequence.•The dolomitic-clastic sequence was suggested to be formed in highly saline environment.•The types of tight oil reservoir and related reservoir spaces were identified.•Secondary pores formed via dissolution of clastics and dolomite by hydrocarbon-related fluids.