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Articles by Guiting Hou
The Formation and Modification of the Arcuate Tectonic Belt in the Northeastern Tibetan Plateau: Insight from Three-Dimensional Finite Element Numerical Simulation
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Study on the structural characteristics of the Yangdachengzi oil layer in the Quantou Formation, ZY block, central depression, Songliao Basin
1College of Energy, Chengdu University of Technology, Chengdu, China 2State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, China 3Research Institute of Petroleum Exploration and Development, Beijing, China 4Oil Production Company of Daqing Oilfield Company Ltd., Daqing, China The Songliao Basin is a large Mesozoic–Cenozoic continental basin with multiple sedimentary cycles.
Impact of mechanical stratigraphy on fracture growth and propagation
1 Introduction Natural fractures are primary seepage channels and effective reservoirs, playing an important role in hydrocarbon migration and accumulation (Zeng et al., 2012; Amjad et al., 2023; Fu et al., 2023).
Analysis of proto-type Tarim Basin in the late Precambrian and the dynamic mechanism of its evolution
(2) Proto-type Tarim Basin in the late Sinian Period. The pattern of rifts distribution in the Sinian Period was inherited from the Nanhua Period, and thus was similar except that these rifts were beginning to shrink. However, the uplift-subsidence pattern of Tarim Basin has changed in the late Sinian Period.
Structures in Shallow Marine Sediments Associated with Gas and Fluid Migration
Abstract : Geological structure changes, including deformations and ruptures, developed in shallow marine sediments are well recognized but were not systematically reviewed in previous studies.
The interactions of fault patterns and stress fields during active faulting in Central North China Block: Insights from numerical simulations
Loading metrics Open Access Peer-reviewed Research Article Bo Shao, Guiting Hou Bo Shao, Guiting Hou Published: April 25, 2019 https://doi.org/10.1371/journal.pone.0215893 Figures Abstract The interaction of active faults as a factor affecting the mechanisms of large earthquakes has been observed in many places. Most aftershock and clustering earthquake sequences do not recur on the main seismogenic fault but are controlled by fault interactions with adjacent seismic structures.
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