Physical simulation experiments of structural deformation and hydrocarbon accumulation in piggyback thrust wedges

Abstract

The piggyback thrust wedge is a common structural style in thrust belts, which controls the lateral arrangement of hydrocarbon distribution. This study conducted physical simulation experiments of structural deformation and hydrocarbon accumulation by using the piggyback thrust wedge as the geological model. According to the experimental results, hydrocarbon accumulation patterns were obtained by investigating the evolutionary history of the fault‐sealing performance while inverting the coupling relationship between the fault evolution and hydrocarbon accumulation. The structural deformation experiment showed that the evolution of the fault displacement and dip angle was characterized by gradual and staged progress. The kaolin smear continuity deteriorated with fault evolution. The soybean oil accumulation experiment demonstrated that the fault‐sealing performance in the rear of the thrust wedge was inferior to that in the front. Hydrocarbon migration was mostly lateral in the front of the thrust wedge and mainly vertical in the rear. Quantitative analysis showed that the fault‐sealing performance had three closed, partially closed, and open stages, which gradually deteriorated with the structural evolution. Three hydrocarbon accumulation patterns were identified in the piggyback thrust wedge: synchronized, adjustment, and non‐adjustment patterns. The evolution of the structural deformation and faults‐sealing performance resulted in spatio‐temporal differences in hydrocarbon accumulation in the thrust belts of central‐western China. The front of the thrust wedge had a higher exploration potential than the rear.

Active Shortening Simultaneous to Normal Faulting Based on GNSS, Geophysical, and Geological Data: The Seismogenic Ventas de Zafarraya Fault (Betic Cordillera, Southern Spain)

“…This active migration likewise affects the evolution of the thrust front, pushing it to propagate in the same trend. Overall, thrusting generally migrates from the inner part toward the outer part of the orogen (Zhao et al., 2022) and develops a piggyback mode of propagation (e.g., Fillon et al., 2013; Ghani et al., 2021; Jia et al., 2020; Ori & Friend, 1984).…”