
Structure, Permeability and Fluid Flow in Sedimentary Clastic Rock Fault Zone
Gong Yajun, Zhang Kuihua, Wang Jinduo, Wang Qianjun, Wang Jianwei, Zeng Zhiping, Guo Ruichao, Niu Jingjing, Fan Jie, Liu Hui, Min Feiqiong
Structure, Permeability and Fluid Flow in Sedimentary Clastic Rock Fault Zone
During the fault growth process, a fault zone with complex three-dimensional structure is formed. The fault zones occupying a very small volume in the Earth’s crust have a significant impact on the migration of fluids within the crust. The study of the interaction between fluids and solids in these fault zones is of great geological and engineering importance. Over the past 30 years, multidisciplinary research has been conducted on the characteristics of fault zones, permeability, and fluid migration patterns in sedimentary clastic rock. However, there is a lack of understanding and efforts in systematically comparing and comprehensively explaining the findings across different disciplines. In this paper, it summarizes the types, formation mechanisms, and geometric characteristics of fault zone. It systematically reviews data on the permeability of fault zones, analyzes three categories of factors influencing permeability changes, and elucidates the fluid migration behavior within fault zones, including dominant pathways, migration velocity, periodic frequencies, critical conditions, and multi-field coupled migration mechanisms. By summarizing the research progress over the past 30 years, in this paper it is expected to deepen our understanding of the complex geological processes of fault-fluid-mineralization. It is important to note that further interdisciplinary collaboration is needed to conduct more in-depth research on the fluid migration within fault zones.
fault / fault zone structure / fault zone permerbility / fluid migration / review / tectonics / petroleum geology
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