Deformation, Diagenesis, and Reservoir in Fault Damage Zone

A special issue of Minerals (ISSN 2075-163X).

Deadline for manuscript submissions: 30 June 2025 | Viewed by 1176

Special Issue Editors


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Guest Editor
School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China
Interests: subduction tectonic; fault analysis; fracture-diagenesis; fractured reservoir

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Guest Editor
PetroChina Exploration and Production Company, Beijing 100007, China
Interests: fractured reservoir; reservoir description; reservoir exploitation

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Guest Editor
School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China
Interests: sedimentology; diagenesis; reservoir evaluation

Special Issue Information

Dear Colleagues,

Fault damage zone, including the narrow fault core and wider damage zone, typically has complicated architecture and a profound impact on the mechanical, hydraulic, and petrophysical properties of the host rocks. There is also fluid activity within the fracture network. The complicated structural–diagenetic process in the fault damage zone significantly influences the architecture and subsequently heterogeneous reservoir along the fault zone. Therefore, geological, geophysical, and engineering technologies have been widely used to detect the architecture, deformation, and reservoir in the fault damage zone. However, there is still a big challenge in deciphering the interaction of the deformation and diagenesis processes, and their effects on the reservoir in the fault damage zone.

This Special Issue, “Deformation, Diagenesis, and Reservoir in Fault Damage Zone”, seeks high-quality works focusing on the latest novel advances in fault damage zones. This Special Issue includes, but is not limited to, the following:

  • Fracture networks and deformation, fluid–rock interaction, and diagenesis and reservoirs in carbonate fault damage zones.
  • The timing and evolution of deformation and diagenesis, interaction between fractures and diagenesis, and the process and evolution of fault damage zones.
  • Methods and technologies, and applications and case studies, in the description of fault damage zones and fractured reservoirs.

Prof. Dr. Guanghui Wu
Prof. Dr. Tongwen Jiang
Dr. Xuefei Yang
Guest Editors

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Keywords

  • fault zone
  • carbonate reservoir
  • deformation
  • fracture network
  • diagenesis
  • fracture–diagenesis interaction

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Published Papers (1 paper)

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Research

16 pages, 9604 KiB  
Article
Differential Characteristics of Conjugate Strike-Slip Faults and Their Controls on Fracture-Cave Reservoirs in the Halahatang Area of the Northern Tarim Basin, NW China
by Shenglei Wang, Lixin Chen, Zhou Su, Hongqi Dong, Bingshan Ma, Bin Zhao, Zhendong Lu and Meng Zhang
Minerals 2024, 14(7), 688; https://doi.org/10.3390/min14070688 - 30 Jun 2024
Viewed by 743
Abstract
The X-type strike-slip fault system and weathering crust karst fracture-cave and channel reservoirs were developed in the Halahatang area of the northern Tarim Basin. However, the relationship between the reservoir and the strike-slip fault remains controversial. Based on the core data, and taking [...] Read more.
The X-type strike-slip fault system and weathering crust karst fracture-cave and channel reservoirs were developed in the Halahatang area of the northern Tarim Basin. However, the relationship between the reservoir and the strike-slip fault remains controversial. Based on the core data, and taking an NE-striking strike-slip fault as an example, this paper dissects the karst reservoir from wells along the strike-slip fault damage zone and analyzes the control of scales, properties, and segmentation styles of strike-slip faults on karst reservoirs. The results show that (1) the scale of the strike-slip fault controls the distribution of the reservoir—the wider the fault damage zone, the wider the fracture-cave reservoirs; (2) the transtensional segments of the strike-slip fault are more likely to produce karstification, and the buried-hill area and the interbedded area are controlled by different hydrodynamic conditions to form different types of karst reservoirs; (3) six different parts of the strike-slip fault are conducive to the formation scale of fault fracture zones. This research provides new insight into recognizing karst reservoirs within strike-slip fault damage zones, which can be further applied to predict karst reservoirs controlled by strike-slip faults. Full article
(This article belongs to the Special Issue Deformation, Diagenesis, and Reservoir in Fault Damage Zone)
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