Controls on the Hydrocarbon Production in Shale Gas Condensate Reservoirs of Rift Lake Basins

Author:

Li Yaohua12,Bi Caiqin2,Fu Chao3,Xu Yinbo2,Yuan Yuan2,Tong Lihua2,Tang Yue2,Wang Qianyou4ORCID

Affiliation:

1. State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 100083, China

2. Oil and Gas Survey, China Geological Survey, Beijing 100083, China

3. Xinjiang Yaxin Coalbed Methane Investment and Development (Group) Co., Ltd., Urumchi 830000, China

4. Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool L69 3GP, UK

Abstract

The production of gas and condensate from liquid-rich shale reservoirs, particularly within heterogeneous lacustrine systems, remains a critical challenge in unconventional hydrocarbon exploration due to intricate multiphase hydrocarbon partitioning, including gases (C1–C2), volatile liquids (C3–C7), and heavier liquids (C7+). This study investigates a 120-meter-thick interval dominated by lacustrine deposits from the Lower Cretaceous Shahezi Formation (K1sh) in the Songliao Basin. This interval, characterized by high clay mineral content and silicate–pyrite laminations, was examined to identify the factors controlling hybrid shale gas condensate systems. We proposed the Hybrid Shale Condensate Index (HSCI), defined as the molar ratios of (C1–C7)/C7+, to categorize fluid phases and address shortcomings in traditional GOR/API ratios. Over 1000 samples were treated by geochemical pyrolysis logging, X-ray fluorescence (XRF) spectrum element logging, SEM-based automated mineralogy, and in situ gas desorption, revealing four primary controls: (1) Thermal maturity thresholds. Mature to highly mature shales exhibit peak condensate production and the highest total gas content (TGC), with maximum gaseous and liquid hydrocarbons at Tmax = 490 °C. (2) Lithofacies assemblage. Argillaceous shales rich in mixed carbonate and clay minerals exhibit an intergranular porosity of 4.8 ± 1.2% and store 83 ± 7% of gas in intercrystalline pore spaces. (3) Paleoenvironmental settings. Conditions such as humid climate, saline water geochemistry, anoxic bottom waters, and significant input of volcanic materials promoted organic carbon accumulation (TOC reaching up to 5.2 wt%) and the preservation of organic-rich lamination. (4) Laminae and fracture systems. Silicate laminae account for 78% of total pore space, and pyrite laminations form interconnected pore networks conducive to gas storage. These findings delineate the “sweet spots” for unconventional hydrocarbon reservoirs, thereby enhancing exploration for gas condensate in lacustrine shale systems.

Funder

National Natural Science Foundation of China

State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum

China Geological Survey

Publisher

MDPI AG

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