Riedel shear structures reactivation may induce earthquakes through long-term steam injection: A case study of a heavy oil production field in northwestern China

Author:

Xu Rui1ORCID,Liang Chuntao2ORCID,KanNi Zhati3,Wang Meijie3,Li Zhongquan4,Wang Chaoliang1,Liu Zhijin1,Chen Chunmei1

Affiliation:

1. Chengdu University of Technology, Key Laboratory of Earth Exploration and Information Techniques, Chengdu, China and Ministry of Education, Chengdu, China.

2. Chengdu University of Technology, Key Laboratory of Earth Exploration and Information Techniques, Chengdu, China; Ministry of Education, Chengdu, China and Chengdu University of Technology, State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu, China. (corresponding author)

3. Xinjiang Oilfield Company, PetroChina, Research Institute of Engineering Technology, Karamay, China.

4. Chengdu University of Technology, State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu, China and Chengdu University of Technology, Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Land and Resource, Chengdu, China.

Abstract

Conventional heavy oil exploitation methods involve steam stimulation and flooding. An oil field in northwestern China has been producing heavy oil via steam injection for several decades. The production area has been seismically quiet until an increase in seismicity occurred several years ago. An array of 40 seismographs has been deployed between July and October 2021 to monitor seismicity and resolve the possible causes of the recent seismicity. Using an end-to-end machine-learning-based high-precision earthquake location workflow, we analyze a microseismic sequence comprised of 178 events that occurred in the study area. Numerical simulations incorporating Coulomb failure stress suggest that prolonged steam injection can reactivate faults and induce seismic events. Similarly, fluid diffusion through conduits may achieve the same effect. Analysis of the focal mechanism solutions of 21 strike-slip and thrust events with [Formula: see text] in conjunction with the background stress regime ([Formula: see text] azimuth = N15°W) reveal that the stress distribution is compatible with a left-lateral Riedel shear structure (RSS) model. Therefore, we can speculate that steam injection may induce earthquakes by reactivating preexisting RSS fault structures. To conclude, the recent seismic events could have been induced by two possible mechanisms: (1) long-term steam injection may cause the static stress level on the faults beneath the reservoir to build up to critical levels, following which a slight stress disturbance can trigger an earthquake and (2) fluid conduits may transport condensed water to basement faults, weakening the faults through fluid diffusion.

Funder

National Natural Science Foundation of China

Publisher

Society of Exploration Geophysicists

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