4.5 Article

Sedimentary Facies Controls for Reservoir Quality Prediction of Lower Shihezi Member-1 of the Hangjinqi Area, Ordos Basin

Journal

MINERALS
Volume 12, Issue 2, Pages -

Publisher

MDPI
DOI: 10.3390/min12020126

Keywords

depositional framework; sedimentary facies; sand-ratio; lower Shihezi member-1; Hangjinqi area

Funding

  1. National Natural Science Foundation of China [4162134, 41820104008]
  2. National Key R & D program of China [2017YFE0106300]
  3. 13th Five year Plan of the Ministry of Science and Technology of China [2016ZX05034-002003]
  4. Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) [CUGCJ1712]
  5. Key Laboratory of Tectonics and Petroleum Resources (China University of Geosciences in Wuhan) [TPR-2018-18]
  6. Yunnan Provincial Government Leading Scientist Program [2015HA024]

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The estimated tight gas reserves in the Hangjinqi area are 700 billion cubic meters. This study focuses on the depositional framework and sedimentary facies analysis of the first member of the lower Shihezi formation. Geological modeling, seismic attributes, and petrophysical modeling are used to identify the presence of braided channels and channel-bars. The results confirm favorable reservoir quality for gas production in the Hangjinqi area.
The tight gas reserves in the Hangjinqi area are estimated at 700 x 109 m(3). Since the exploration of the Hangjinqi, numerous wells are already drilled. However, the Hangjinqi remains an exploration area and has yet to become a gas field. Identifying a paleo-depositional framework such as braided channels is beneficial for exploration and production companies. Further, braided channels pose drilling risks and must be properly identified prior to drilling. Henceforth, based on the significance of paleochannels, this study is focused on addressing the depositional framework and sedimentary facies of the first member (P(2)x(1)) of the lower Shihezi formation (LSF) for reservoir quality prediction. Geological modeling, seismic attributes, and petrophysical modeling using cores, logs, interval velocities, and 3D seismic data are employed. Geological modeling is conducted through structural maps, thickness map, and sand-ratio map, which show that the northeastern region is uplifted compared to northwestern and southern regions. The sand-ratio map showed that sand is accumulated in most of the regions within member-1. Interval velocities are incorporated to calibrate the acoustic impedance differences of mudstone and sandstone lithologies, suggesting that amplitude reflection is reliable and amplitude-dependent seismic attributes can be employed. The Root Mean Square (RMS) attribute confirmed the presence of thick-bedded braided channels. The results of cores and logging also confirmed the presence of braided channels and channel-bars. The test results of wells J34 and J72 shows that the reservoir quality within member-1 of LSF is favorable for gas production within the Hangjinqi area.

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