Genesis of diagenetic zeolites and their impact on reservoir formation in the Middle Permian Lower-Wuerhe Formation of the Mahu Sag, Junggar Basin, Northwest China

Abstract

Zeolites are important diagenetic minerals in petroleum reservoirs and have complex impacts on reservoir quality. To highlight this critical and challenging issue, we conduct a case study in the Middle Permian Lower-Wuerhe Formation in the Mahu Sag, Junggar Basin, China. Formation mechanism of zeolites and their impacts on the reservoir quality. Our results show that there are five types of zeolite minerals (i.e. laumontite, heulandite, analcime, stilbite, and clinoptilolite) in the Lower-Wuerhe Formation reservoir, with laumontite and heulandite being the main types. Petrographic and geochemical data suggested that laumontites developed in the Lower-Wuerhe Formation were mainly precipitated from pore water, whereas heulandites were formed associated with alteration of volcanic materials. In addition, the distribution of different type of zeolite minerals is generally controlled by sedimentary facies. The heulandite–laumontite zone developed mainly in the front of fan-delta plain, and the laumontite zone developed mainly in fan-delta front. The distal part of fan-delta front is dominated by albite. The zeolite mineral assemblages are generally controlled by geochemical composition of volcanic lithic fragments. The high content of intermediate-basic volcanic lithic fragments in the eastern Mahu Slope sediments is responsible for authigenic minerals such as heulandite, chlorite, and laumontite. However, the content of intermediate-basic volcanic lithic fragments in the western Mahu Slope sediments is low which results in the cement in this region is dominated by laumontite and mixed-layer illite/smectite. In general, conglomerates deposited in fan-delta front are favorable for the formation of early laumontite and late dissolution of laumontite due to resistance to compaction by coarse fraction and accumulation of acidic fluids in structural highs, which resulted in the formation of a high-quality reservoir. Our results have general implications for hydrocarbon exploration of the zeolite-bearing conglomerate reservoirs in non-marine petroliferous basins.

Characteristics and Genesis of Pore–Fracture System in Alkaline Lake Shale, Junggar Basin, China

“…The Fengcheng Formation consists of the first member of the Fengcheng Formation (P 1 f 1 ), the second member of the Fengcheng Formation (P 1 f 2 ), and the third member of the Fengcheng Formation (P 1 f 3 ) from the bottom up, with a thickness of about 800-1800 m and a burial depth of more than 4000 m. It is mainly deposited in lacustrine facies, mostly shale and occasionally siltstone interlayers, and the whole is dominated by dark fine-grained sedimentary dolomitic shale and siliceous shale. It is the oldest alkali-lake source rocks in the world [25].…”

“…about 800-1800 m and a burial depth of more than 4000 m. It is mainly deposited in lacustrine facies, mostly shale and occasionally siltstone interlayers, and the whole is dominated by dark fine-grained sedimentary dolomitic shale and siliceous shale. It is the oldest alkali-lake source rocks in the world [25].…”