Tectonics (Posters) I: Strike-slip, Extension, Alpine-Himalayan TectonicsSeattle Annual Meeting
Etna, is speckled by volcanics and strongly affected by strike-slip tectonics. Transpressive deformation produced a push-up and a remarkable shortening along WNW-ESE to NW-SE trending lineaments. Fault segments, bounding basinal areas, show evidence of positive tectonic inversion, suggesting a ...
Post-Late Cretaceous Strike-Slip Tectonics and Its Implications for the Southeast Anatolian Orogen, Turkey. International Geology Review 38, 818-831.YIqGbIqTBASc, E. & YILMAZ, Y. 1996b. Post-Late Creta- ceous strike-slip tectonics and its implications for the Southeastern Anatolian orogen, ...
Famenno-Carboniferous (370-320 Ma) Strike Slip Tectonics Monitored By Syn-kinematic Plutons In The French Variscan Belt (Massif Armoricain And French Massif Central) 作者: Marquer, Didier;Cocherie, Alain;Rolin, Patrick;Cartannaz, Charles;Rossi, Philippe;Thiery, Vincent;Quenardel, Jean-Michel;...
3.The weaknesses, difficulties and key points of the present study of basin tectonic dynamics are shown in the following four aspects: (1)Tectonics with complex features and complex cause of formation, such as strike-slip structure, lateral trans.目前盆地构造动力学研究的弱点、难点及重点主要有以下...
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...
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 ...
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 zones in the area, including those of Upper Elbe, Intra-Sudetic, Odra, Dolsk and Kraków-Lubliniec. These faults are...
The weaknesses, difficulties and key points of the present study of basin tectonic dynamics are shown in the following four aspects: (1)Tectonics with complex features and complex cause of formation, such as strike-slip structure, lateral trans. ...