Abstract
The shale layers of the Permian Shanxi Formation and Taiyuan Formation in the southwestern part of Shandong Province are marine-continental transitional sedimentary facies. When compared with the Ordos Basin, which was a typical breakthrough in marine-continental transitional shale gas exploration, the geological characteristics, exploration, and development prospects of marine-continental transitional shale gas in the southwestern section of Shandong Province are more defined. The shale gas deposits of the Shanxi and Taiyuan Formations in southwestern Shandong Province have the following geological characteristics. The sedimentary environments of Shanxi and Taiyuan Formations are considered to be stable and characterized with widely distributed organic-rich shale, which can be used as composite evaluation layers. The total thickness of the shale range is between 140 and 350 m, with an average of 230 m. The main types of organic matter in the Shanxi Formation are Type Ⅲ and Type Ⅱ2 kerogen, while the main types of organic matter in the Taiyuan Formation are rock types. The abundance and maturity of the organic matter are high, and the gas generating capacity is strong. The reservoir rock mineral composition is complex in the region. The clay mineral content is relatively high and the brittle mineral content is rich. Also, the shale fracturing ability is good. The region has the characteristics of a low porosity and low permeability reservoir, with relatively good reservoir capacity. Three primary points of interest have stably been developed within the region, which are located in the upper high water level system, near the initial flood surface, and the majority of flood surface, including a transgressive system tract and high level system tract. The total gas content is estimated to range between 0.03 and 4.47 m3/t, with an average of 0.30 m3/t. The shale gas resources are rich, including one favorable Class I location with an area of 819.06 km2 and a resource amount of 985.84 × 108 m3; four favorable Class Ⅱ locations with an area of 1,979.68 km2 and a resource amount of 2,278.14 × 108 m3; and five prospective locations with an area of 8,385.52 km2 and a resource amount of 7,299.48 × 108 m3. Therefore, the region was considered to have major exploration potential.
Highlights
Outside of North America, China is currently the largest shale gas producer in the world
Adsorbed gas occurs on the surfaces of organic matter or clay minerals, and free gas occurs in matrix pores and cracks (Zhang et al, 2004; Zou et al, 2010)
This study found that when compared with the Ordos Basin, the shale of the Shanxi and Taiyuan Formations in the study area had displayed similar geological characteristics which could potentially indicate rich shale gas resources and major development potential
Summary
Outside of North America, China is currently the largest shale gas producer in the world. It is expected that with the continuing breakthroughs which are being made in domestic shale gas exploration and development, the development potential and prospects of shale gas will attract significant attention from researchers (Zou et al, 2021). Shale gas is a type of unconventional natural gas which exists mainly in either an adsorbed or free state. Shale gas is self-generating and selfstoring and continually accumulates in shale deposits. Adsorbed gas occurs on the surfaces of organic matter or clay minerals, and free gas occurs in matrix pores and cracks (Zhang et al, 2004; Zou et al, 2010). Shale gas reservoirs’ storage and fluid permeability characteristics are highly valued
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