The Tight Sand Reservoir Characteristics and Gas Source in Coal Measures: A Case Study of Typical Areas in China

Author:

Liu Zengqin12ORCID,Guo Shaobin3,Huang Yiming4,Cao Zhe1,Yeerhazi Talihaer·3,Cao Weifu5

Affiliation:

1. Petroleum Exploration and Production Research Institute, Sinopec, Beijing 102206, China

2. Sinopec Key Laboratory of Shale Oil/Gas Exploration and Production, Beijing 102206, China

3. School of Energy Resources, China University of Geosciences, Beijing 100083, China

4. No.1 Oil Production Plant, Daqing Oilfield Co., Ltd., Daqing 163001, China

5. Exploration and Development Research Institute, PetroChina Daqing Oilfield Company, Daqing 163712, China

Abstract

Interbedded sandstones, shales, and coal seams were formed in marine-continental transitional environments of coal measures, and the gas source of its tight sand gas has been uncertain, which hinders the progress of natural gas exploration. This article uses the Longtan tight sand gas in west Guizhou as an example to investigate the reservoir features, gas charging history, and main source rock of tight sand gas by examining thin sections, scanning electron microscopy images, X-ray diffraction results, and the fluid inclusions with burial and thermal histories and noble gas analysis. The Longtan sandstones in this study are classified as litharenites which are characterized by low compositional and textural maturities, and high clay contents, and are distinguished petrographically from conventional sandstones by the extensive existence of micropores and microfractures. The results of the homogenization temperatures of the fluid inclusions show that the Longtan tight sand gas is a single-stage accumulation which occurred during the Late Triassic. Furthermore, through the analysis of the helium and argon isotopes of noble gases, a calculation model was established for determining the shale and coal contributions to the tight sand gas. The research results show that the Longtan tight sand gas mainly belongs to the crust-derived gas, mostly from the Longtan shale-derived contribution and to a lesser extent from the Longtan coal-derived contribution. The measured 40Ar/36Ar values of the Longtan shales and coals are consistent with the forecasted 40Ar/36Ar values from the calculation model, demonstrating that the model is viable to calculate the source rock contribution to the tight sand gas. Therefore, the Longtan shales as main source rocks can generate hydrocarbons to charge neighboring tight sandstones to form tight gas accumulation in the Longtan Formation, which provides an opportunity for tight gas development in west Guizhou.

Funder

Ministry of Science and Technology of the People's Republic of China

Publisher

Hindawi Limited

Subject

General Earth and Planetary Sciences

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