This lineation of shallow earthquakes and volcanic activity is attributed to five corresponding normal faults which are named after the five corresponding volcanic centers (Sousaki, Methana, Milos, Santorini and Nisyros). This is supported by a similar trend of the geomorphological features (grabens ...
1, L3 and L4), and whether the faults that bound the relay zones connect into a single plane (Fig. 1, L2 and L3) or are unconnected in 3D (Fig. 1, L1 and L4). Fig. 1(L5-L8) shows more complicated arrays with various combinations of different types of relay zone. These examples...
We present a conceptual model to explain the development of damage zones around faults in high-porosity sandstones. Damage zone deformation has been partic... ZK Shipton,PA Cowie - 《Journal of Structural Geology》 被引量: 283发表: 2003年 Effect of faulting on fluid flow in porous sandstones:...
along low-angle normal faults i n the brittle upper crust. Theories to resolve the seismicity paradox fal l into two categori es: those that do not require brittle slip at low angl es (e.g. “rol ling hinge” model [Wernicke and Axen, 1988] and ...
At greater depths, fault dip angles are unclear in the marine seismic surveys. Together, these results can be interpreted as curved or listric faults, with steeply dipping near the surface and leveling off with depth. Therefore, we made a new fault model that consisted of an upper half with...
Possible seismogenic shallow-dipping normal faults in the Woodlark-D’Entrecasteaux extensional province, Papua New Guinea. Geology 19, 1205–1208 (1991). Google Scholar Abers, G. A., Mutter, C. Z. & Fang, J. Shallow dips of normal faults during rapid extension: earthquakes in the Wood...
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(blue), or negligible uplift across IN-EU collision zone from GPS observations (dots) and paleoelevation studies (numbered diamonds). Numbers are listed with corresponding citations and associated uplift rates. Gray-scale, black symbols, and teal lines represent topography, major faults, and rivers...
In particular, quantitative methods are still lacking in the literature to critically assess the accuracy of T-D plots and ancillary T-Z data when interpreting faults at different scales. Show abstract Structural Inheritance and Rapid Rift-Length Establishment in a Multiphase Rift: The East Green...
The Skinos Relay domain drains to sea level, lying on the relay ramp between the closely spaced Kamarissa and Skinos Faults. Here, interaction between the displacement fields associated with each of the closely spaced faults controls the rate and style of landscape evolution. In contrast to ...