Shear zones–A review
Strain in the lithosphere localizes into tabular zones known as shear zones that grow from
small outcrop-size individual zones to large composite structures. Nucleation is related to …
small outcrop-size individual zones to large composite structures. Nucleation is related to …
[HTML][HTML] Structural inheritance in amagmatic rift basins: Manifestations and mechanisms for how pre-existing structures influence rift-related faults
In the context of rift basin formation, structural inheritance describes the influence of pre-
existing structures on new rift-related structures, including faults. Pre-existing structures in …
existing structures on new rift-related structures, including faults. Pre-existing structures in …
[LIVRE][B] The mechanics of earthquakes and faulting
CH Scholz - 2019 - books.google.com
This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …
Location of largest earthquake slip and fast rupture controlled by along‐strike change in fault structural maturity due to fault growth
Earthquake slip distributions are asymmetric along strike, but the reasons for the asymmetry
are unknown. We address this question by establishing empirical relations between …
are unknown. We address this question by establishing empirical relations between …
Segmentation and growth of an obliquely reactivated normal fault
Detailed kinematic analysis of a large (1800 m maximum displacement) reactivated normal
fault in the Taranaki Basin, New Zealand, has been conducted using high quality 3D seismic …
fault in the Taranaki Basin, New Zealand, has been conducted using high quality 3D seismic …
Fault trace corrugation and segmentation as a measure of fault structural maturity
As faults grow over time and become more “mature,” some of their geometrical and
mechanical properties evolve, and these changes modify earthquake behavior. It is thus of …
mechanical properties evolve, and these changes modify earthquake behavior. It is thus of …
How do normal faults grow?
Normal faults grow via synchronous increase in displacement and length ('propagating fault
model', also known as the 'isolated fault model'), or by rapid length establishment and …
model', also known as the 'isolated fault model'), or by rapid length establishment and …
Two-phase Cretaceous–Paleocene rifting in the Taranaki Basin region, New Zealand; implications for Gondwana break-up
The break-up of Gondwana resulted in extension of New Zealand continental crust during
the Cretaceous–Paleocene. Offshore the geometry and rift history are well imaged by new …
the Cretaceous–Paleocene. Offshore the geometry and rift history are well imaged by new …
Integrating 3D seismic interpretation, well log analysis and static modelling for characterizing the Late Miocene reservoir, Ngatoro area, New Zealand
The late Miocene thick accumulations of submarine fan and slope fan deposits namely the
Mount Messenger Formation, represent low resistivity reservoir within Taranaki Basin of …
Mount Messenger Formation, represent low resistivity reservoir within Taranaki Basin of …
Techniques to determine the kinematics of synsedimentary normal faults and implications for fault growth models
Normal faults grow via a sympathetic increase in their displacement and length ('isolated
model') or by rapid establishment of their near-final length prior to significant displacement …
model') or by rapid establishment of their near-final length prior to significant displacement …