Title Deep shale gas in the Ordovician-Silurian Wufeng-Longmaxi formations of the Sichuan Basin, SW China: Insights from reservoir characteristics, preservation conditions and development strategies
Authors Nie, Haikuan
Jin, Zhijun
Li, Pei
Katz, Barry Jay
Dang, Wei
Liu, Quanyou
Ding, Jianghui
Jiang, Shu
Li, Donghui
Affiliation State Key Lab Shale Oil & Gas Enrichment Mech & Ef, Beijing 102206, Peoples R China
Sinopec Petr Explorat & Prod Res Inst, Beijing 102206, Peoples R China
Peking Univ, Inst Energy, Beijing 100871, Peoples R China
Chevron CTC, 1500 Louisiana St, Houston, TX 77002 USA
Xian Shiyou Univ, Sch Earth Sci & Engn, Xian 710065, Peoples R China
CNPC Engn Technol R&D Co Ltd, 5 Huanghe Rd, Beijing 102206, Peoples R China
China Univ Geosci, Sch Earth Resources, Wuhan 430074, Peoples R China
China Petr & Chem Corp SINOPEC, Petr Explorat & Prod Res Inst, 197 Baisha Rd, Beijing 102206, Peoples R China
Keywords FORT-WORTH BASIN
THERMAL MATURITY
DISTRIBUTION PATTERN
GEOLOGICAL CONTROLS
BARNETT SHALE
EXPLORATION
ENRICHMENT
LITHOFACIES
MECHANISMS
GENERATION
Issue Date 1-Apr-2023
Publisher JOURNAL OF ASIAN EARTH SCIENCES
Abstract Shale gas at a burial depth greater than 3500 m is an important potential strategic target for exploration and development in China. Due to the complex geological and engineering settings, our understanding of the enrichment and retention mechanisms of deep shale gas is limited, and large-scale commercial development has not yet been realized. In this study, deep shale gas in the Upper Ordovician Wufeng Formation and Lower Silurian Longmaxi Formation of the Sichuan Basin is systematically studied in terms of the spatial distribution of black shale, reservoir types and properties, preservation conditions, and gas content as well as exploration and development practices. The deep siliceous shale of the Dicellograptus complexus-Cystograptus vesiculosus biozone exhibits high quartz content, which is conducive to the formation and preservation of effective reservoirs, thus it is often recognized as the optimal interval for deep shale gas development. Compared with the shallower res-ervoirs, microfractures in deep shale gas reservoirs are not developed. Also, overburden pressure and high temperature bring about a 40 %-50 % reduction in porosity and an 80 %-90 % decrease in permeability. High formation temperature, large in-situ stress and high-stress difference between the horizontal stress and vertical stress in the deep shale gas reservoirs lead to elevated shale plasticity, making it difficult to form and extend fracture. Moreover, due to the high fracture closure pressure, proppant tend to easily break in addition to the reduction of effective hydraulic fractures and fracture conductivity, which explains why it is difficult to effec-tively fracture deep shale and to achieve high and stable gas production. It is recommended to establish a volume fracturing plan (such as a long horizontal well with an increasing number of stages and perforations) for certain deep shale gas reservoirs. Creating and optimizing reasonable production systems with excellent pressure management procedures are also crucial to maximize deep shale gas production and ultimately realizing the commercial development of deep shale gas.
URI http://hdl.handle.net/20.500.11897/671058
ISSN 1367-9120
DOI 10.1016/j.jseaes.2022.105521
Indexed SCI(E)
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