Xinjiang Petroleum Geology ›› 2025, Vol. 46 ›› Issue (4): 395-402.doi: 10.7657/XJPG20250401

• OIL AND GAS EXPLORATION •     Next Articles

Exploration History and New Frontiers of Oil and Gas in Deep to Ultra-Deep Carbonate Reservoirs in Tarim Basin

CAO Zicheng1(), GENG Feng2, REN Lidan2, JIANG Huashan1, SHANG Kai2, LIU Yongli2   

  1. 1. Northwest Oilfield Company, Sinopec, Urumqi, Xinjiang 830011, China
    2. Research Institute of Exploration and Development, Northwest Oilfield Company, Sinopec, Urumqi, Xinjiang 830011, China
  • Received:2024-12-31 Revised:2025-01-23 Online:2025-08-01 Published:2025-07-25

Abstract:

Deep to ultra-deep carbonate reservoirs have become a critical component for increasing hydrocarbon reserves and production in the Tarim Basin, and represent a pivotal direction for future exploration. This paper systematically reviews the geological theories of hydrocarbon accumulation and summarizes the exploration achievements in the Tarim Basin. The exploration of deep to ultra-deep marine carbonate reservoirs in the Tarim Basin can be primarily divided into four stages: the buried-hill reservoir exploration stage (1984-1996), the karst fractured-vuggy reservoir exploration stage (1997-2015), the fault-controlled fractured-vuggy reservoir exploration stage (2016-2020), and the new frontier and new type reservoir exploration stage (2021-present). Through an integrated analysis on geological conditions, exploration trends, and potential reserves-enhancing areas, several key prospects were identified, including fault-controlled fracture-cavity zones in the Shunbei area, multi-type fracture-cavity zones in the Tabei area, composite fracture-cavity zones in the Tazhong area, composite fracture-cavity zones in the Maigaiti slope, and deep Sinian-Cambrian dolomites in the western margin of the Manjiaer depression.

Key words: Tarim Basin, deep to ultra-deep stratum, carbonate rock, exploration history, resource potential, geological condition, typical oil and gas reservoir, new exploration frontier

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