Strike-slip tectonics has been the dominant style of deformation during the neotectonic (Pliocene and Quaternary) evolution of the Pannonian basin. Main faults are exposed in the "island mountains" of the basin, but strike-slip tectonic features can be best studied in the basin fill by seismic...
aflexural loading flexural装货[translate] adoyouknowthis? doyouknowthis ?[translate] a1JHh2MZbHhnQwZun5B2GSE3VjvNaKyW8gR 1JHh2MZbHhnQwZun5B2GSE3VjvNaKyW8gR[translate] aconvergent and strike-slip tectonics 会聚和触击滑倒构造[translate]...
Neogene Quaternary strike-slip tectonics in the central Calabria Arc (southern Italy), J. Geodyn., 43, 397 414.C. Tansi, F. Muto and S. Critelli, "Neogene-Quaternary Strike-Slip Tectonics in the Central Calabrian Arc (South- ern Italy)," Journal of Geodynamics, Vol. 43, No. 3, 2007...
Strike-slip tectonics and granite petrogenesis 来自 掌桥科研 喜欢 0 阅读量: 95 作者:DHW Hutton,RJ Reavy 摘要: Transpression is a process that thickens the crust and therefore in obliquely convergent orogens as in normally convergent orogens there is the potential to generate granitic melts. ...
We present a variety of models for strike-slip tectonics which represent a useful database for seismic interpreters and geologists. In pure strike-slip, the Riedel shear geometry is shown to depend on the initial stress state, interference of parallel basement faults and horizontal layering of the...
173 STRIKE-SLIP AND OBLIQUE-SLIP TECTONICS Strike–slip faulting is a common mode of deformation in both continental and oceanic crust and occurs at a wide range of scales. Strike slip systems are relatively narrow and subvertical wrench zones along which two adjacent blocks move sideways, horizon...
Seismic, structural, and stratigraphic analyses reveal that the strike-slip rift system in West and Central Africa represents a new type: the intraplate divergent strike-slip fault system. This system is related to the pre-existing tectonics of the African basement, the breakup of Gondwana, the ...
Based on these data, two alternative concepts explaining the connection of the Variscan belt and its NE foreland, those of strike-slip tectonics versus oroclinal bending, are discussed. The WNW–ESE structural trend in the Variscan foreland is parallel to a set of major strike-slip fault ...
Eastern Hunan-western Jiangxi(EHWJ) is an important site of Tan-Lu fault south elongation.Since Mesozoic Era the NNE-trending left-lateral strike-slip tectonics (NNE-SST) are mainly compounded of T3～ J convergent SST and K～ E divergent SST. The convergent strike-slip faulting resulted in ...
Structural studies carried out in the Lucanian Apennines (Southern Italy) show that strike-slip faulting was the principal mode of deformation of this area during middle-upper Pleistocene time. W-NW to E-SE trending left strike-slip fault systems dissect the entire Apennine mountain belt and affe...