在系统回顾走滑断裂研究历史, 形成机制和基本构造特征的基础上, 重点讨论了我国大型克拉通
叠合盆地走滑构造与油气聚集方面的最新研究进展. 概括起来包括:(1) 走滑断裂应力和生长机制 …

Seismic mapping of subsurface faults is hampered by factors such as seismic resolution,
velocity control for depth conversion and human bias. Here, we explore the challenges and …

Faults are complex structures that substantially influence the mechanical behavior and
hydraulic connectivity of rock formations. Therefore, studying faults is important for a variety …

Damage zones of different fault types are investigated in siliciclastics (Utah, USA),
carbonates (Majella Mountain, Italy) and metamorphic rocks (western Norway). The study …

活动断裂带强烈复杂的构造运动会对地壳岩体产生不同程度的损伤, 这些损伤能够显著影响地震
破裂, 地貌演化和地质灾害等地质过程, 并对工程岩体稳定有较大影响, 但目前鲜见对大型活动 …

We studied the geometry and petrophysical properties of fault core and damage zones of a
deformation band fault zone in the arkosic sandstones of the Cretaceous Antenor Navarro …

Fault core accommodates intense deformation in the form of slip surfaces and fault rocks
such as fault gouge, cataclasite, breccia, lenses, shale smear, and diagenetic features. The …

Faults with throws that fall below vertical seismic resolution are challenging to identify in
reflection seismic datasets. Nevertheless, such small-scale faults may still affect the seismic …

Faults are characterized by a complex internal architecture. In carbonates, the geometry,
attitude, and distribution of fault-related fractures and subsidiary faults can largely affect the …

In permeability modeling of fault damage zones affecting porous sandstones, deformation
bands are commonly considered low-permeability structures that influence fluid flow …