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Data from: Brittle sedimentary strata focus a multimodal depth distribution of seismicity during hydraulic fracturing in the Sichuan basin, southwest China

An, Mengke1; Elsworth, Derek2; Zhang, Fengshou3; Li, Junlun4; Xu, Zhengyu5; Zhong, Zhen6; He, Manchao7

Published Jan 17, 2024; Updated Jan 28, 2024 on Dryad. https://doi.org/10.5061/dryad.cvdncjt9p

Data files

Jan 17, 2024 version files 4.09 MB
Jan 28, 2024 version files 4.09 MB

Abstract

The number of background earthquakes (ML ≥ 0) in the southern Sichuan basin, southwest China, has increased thirtyfold as a result of hydraulic fracturing. Background events are originally deep (4-6 km) within the sedimentary section but build into a multimodal distribution both at depth and in the shallow stimulated reservoir (2-4 km) - representing a counterpoint to the usual triggering of seismicity on deep sub-reservoir basement faults. Surprisingly, the largest events (ML ≥ 3) evolve in the deep sedimentary strata (4-6 km) that are hydraulically isolated from the injection zone (2-4 km) by low permeability layers. We evaluate the friction-stability rheology of the strata within the full stratigraphic section to define the feasibility of nucleation within these shallow and deep strata. These show velocity-neutral to velocity-weakening behavior in the shallow reservoir transitioning to more strongly velocity-weakening with increase in both depth and temperature. Poroelastic stress calculations confirms that stress transfer, rather than transmitted fluid pressures, are capable of directly reactivating critically-stressed faults at depth, with fluid pressures the triggering source within the shallow reservoir.