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Strike-Slip

On the geoelectric structure of major strike slip faults and shear zones

On the geoelectric structure of major strike slip faults and shear zones

... teristic features that might be observed in a major strike-slip fault zone (Figs. 4 and 5). Model sz-12 shows a 1 ohm- m fault zone conductor (FZC) that extends to 5 km, simi- lar to that observed at ...

8

A finite rectangular strike slip fault in a linear Viscoelastic half space creeping under tectonic forces

A finite rectangular strike slip fault in a linear Viscoelastic half space creeping under tectonic forces

... rectangular strike slip fault of finite length has been taken to be situated in a linearly viscoelastic half space representing the Lithosphere-Asthenosphere ...

9

Strike slip motion of a mega splay fault system in the Nankai oblique subduction zone

Strike slip motion of a mega splay fault system in the Nankai oblique subduction zone

... the slip rate of the WBSF from the offset of Shionomisaki Canyon (Figure ...of strike-slip along the WBSF can be calculated as approximately 3 mm/year by divid- ing the offset length by the age (=6 ...

14

New Insights on the Role of the Strike Slip Tectonics in the Late Miocene Quaternary Evolution of Sicily

New Insights on the Role of the Strike Slip Tectonics in the Late Miocene Quaternary Evolution of Sicily

... The strike-slip tectonics thus controlled the deposition of different sedimentary cycles on the thrust-top basins and governed the tectonic inversion of the external sectors of the Africa pa- ...

20

Deformation of a two phase medium due to a long buried strike slip fault

Deformation of a two phase medium due to a long buried strike slip fault

... The elastic residual field due to a strike-slip fault in various Earth models has been calculated by several in- vestigators e.g. [1-12] and others. In [1], the problem of the static deformation of a ...

6

Combined uranium series and 10Be cosmogenic exposure dating of surface abandonment: A case study from the Ölgiy strike-slip fault in western Mongolia

Combined uranium series and 10Be cosmogenic exposure dating of surface abandonment: A case study from the Ölgiy strike-slip fault in western Mongolia

... This is a repository copy of Combined uranium series and 10Be cosmogenic exposure dating of surface abandonment: A case study from the Ölgiy strike-slip fault in western Mongolia.. White[r] ...

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The 2018 Hokkaido Eastern Iburi earthquake (MJMA = 6 7) was triggered by a strike slip faulting in a stepover segment: insights from the aftershock distribution and the focal mechanism solution of the main shock

The 2018 Hokkaido Eastern Iburi earthquake (MJMA = 6 7) was triggered by a strike slip faulting in a stepover segment: insights from the aftershock distribution and the focal mechanism solution of the main shock

... Qualitatively, these motions possibly promoted reverse faulting in the northern and southern segments. To test the fault model, the Coulomb failure stress change (ΔCFS) in and around the focal area was calculated (see ...

8

The role of mechanical stratigraphy on the refraction of strike-slip faults

The role of mechanical stratigraphy on the refraction of strike-slip faults

... Abstract. Fault and fracture planes (FFPs) affecting multi- layer sequences can be significantly refracted at layer–layer interfaces due to the different mechanical properties of the contiguous layers, such as shear ...

14

Analogue modelling of strike slip surface ruptures: Implications for Greendale Fault mechanics and paleoseismology

Analogue modelling of strike slip surface ruptures: Implications for Greendale Fault mechanics and paleoseismology

... There are two separate fault morphologies represented by the experiments in this study, and they represent the Greendale Fault at different scales. This interpretation is supported by clear morphological differences ...

158

Formation of Extensional Basin in Internal Part of the Zag Ros Orogeny in West of Sirjan, Iran

Formation of Extensional Basin in Internal Part of the Zag Ros Orogeny in West of Sirjan, Iran

... of strike slip faults are more dextral type and less sinistral which cut and displaced the thrusts of study area and their characteristics conformed to tear ...dextral strike slip faults ...

7

Tectonic history of the Los Angeles Basin: Understanding what formed and deforms the city of Los Angeles

Tectonic history of the Los Angeles Basin: Understanding what formed and deforms the city of Los Angeles

... region contributed to the formation and subsidence of the LA Basin. It seems that both extensional rifting due to large-scale clockwise rotation of crustal blocks and simultaneous dextral strike-slip ...

14

Attenuation Relations of Strong Motion in Japan Using Site Classification Based on Predominant Period

Attenuation Relations of Strong Motion in Japan Using Site Classification Based on Predominant Period

... The PGAs predicted by the crustal and interface models are compared with data from crustal and interface earthquakes of magnitude 6.0 or larger in Figure 2(a). The PGA data have been normalized to magnitude 7.0, a focal ...

12

Sourcing of Miocene accretionary lapilli on ‘Eua, Tonga; atypical dispersal distances and tectonic implications for the central Tonga Ridge

Sourcing of Miocene accretionary lapilli on ‘Eua, Tonga; atypical dispersal distances and tectonic implications for the central Tonga Ridge

... Dispersal within ocean-surface pyroclastic density currents is supported but strike-slip movement in a fault zone south of ‘Eua, post Middle Miocene but pre ridge-splitting, can account [r] ...

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Geological and Geophysical Studies of the Atacama Fault Zone in Northern Chile

Geological and Geophysical Studies of the Atacama Fault Zone in Northern Chile

... Plate Motions and Strike-Slip Faulting We have seen that sea floor spreading and plate tectonics imply continuing motion of a lithospheric plate toward the trench, more or less normal to[r] ...

287

Striations on minor faults and the structure of the
Parmeener Super group near Hobart, Tasmania

Striations on minor faults and the structure of the Parmeener Super group near Hobart, Tasmania

... system implies this area is distant from large scale strike slip faults but the dominance of very steep fault planes implies that many of the extensional faults occur on pre-existing fra[r] ...

7

A detailed seismic zonation model for shallow earthquakes in the broader Aegean area

A detailed seismic zonation model for shallow earthquakes in the broader Aegean area

... Arc. Strike-slip focal mechanisms are mainly recognized in the North Aegean, the Marmara Sea and the northwestern part of Turkey, following the North Anatolia fault branches and its continuation in the ...

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Utsu aftershock productivity law explained from geometric operations on the permanent static stress field of mainshocks

Utsu aftershock productivity law explained from geometric operations on the permanent static stress field of mainshocks

... largest strike-slip mainshocks in southern California (with first-generation aftershocks only; the den- sity distribution comprising all aftershocks generated by the Lan- ders mainshock is represented by ...

10

A fault and seismicity based composite simulation in northern California

A fault and seismicity based composite simulation in northern California

... A number of fault-based simulations of seismicity have been carried out. A limited simulation model for earthquakes on specified strike-slip faults in California called Virtual Cal- ifornia (VC) was given ...

12

Stratiform and Strata Bound Zn Pb Ag Deposits in
Proterozoic Sedimentary Basins, Northern Australia

Stratiform and Strata Bound Zn Pb Ag Deposits in Proterozoic Sedimentary Basins, Northern Australia

... The major stratifonn Zn-Pb-Ag deposits exhibit many similar geological and geochernical features that include: 1 location close to regionally extensive normal and strike-slip synsedirnen[r] ...

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Investigation of lithospheric structure in Mongolia fault: InSAR observations and modelling

Investigation of lithospheric structure in Mongolia fault: InSAR observations and modelling

... The Earth’s mantle is a viscoelastic material (Thatcher and Pollitz, 2008). It flows like a very viscous fluid on long time scales. Large magnitude earthquakes change the stresses in the crust and upper mantle. Aseismic ...

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