Active faults related to active folding and active folds are discussed based on aerial pho- tographs interpretation, detailed topographic analysis, and geologic surveys in the Toka- machi Basin on the middle reaches of the Shinano River. A fight of terraces formed Since 0.5Ma is widely ...
2003. Active Faults and Related Late Quaternary Deformation along the Northweastern Himalayan Frontal Zone, India. Analysis of Geophysics 46: 917-936.Malik JN, Nakata T (2003) Active faults and related late Quaternary deformation along the northwestern Himalayan frontal zone, India. Ann Geophys 46...
There, the Pliocene-to-present units are faulted and folded, indicating that tectonic activity is still on-going, thus contributing to the local seismic hazard. Top-to-the NE and SW normal faults are common in the area and deform the Pliocene-to-present succession together with NE-SW strike...
Notably, some major faults, including the Yangsan and Ulsan fault zones, are relatively misoriented to slip under the current stress condition but, paradoxically, have more (paleo-)seismic records indicating their role in accommodating the neotectonic transpressional strain. We propose that fluids,...
High-resolution digital elevation data (TOPSAR 10-m grid) are used to reconstruct Late Quaternary growth histories of subtle folding in the Wairarapa fold-and-thrust belt, North Island, New Zealand. Outcrop data of deformed latest Miocene and younger strata are combined with observations of warped...
These observations indicate that the fault remained active from the Pliocene to the Quaternary, and possibly up to the present time. How- ever, the estimates of the minimum slip rate on the faults of about 0.02 mm a-1 vertical and 0.03 mm a-1 horizontal are unlikely to produce any ...
Since the GOM is an old rift basin, the transfer faults are generally regarded as little more than tectonically inactive remnants on a passive margin. The post rifting tectonics of the GOM are largely described in terms of growth faulting related to deltaic progradation, salt tectonics, and ...
Recent morphotectonic investigations and our field observations in the area have also shown that all the faults of the study area are tectonically active and show distinct geomorphic signatures such as folding and tilting of terraces, development of strath terraces, triangular fault facets, drainage an...
The layer of sediments above the salt layer is confined into a complex system of faults which is mainly oriented subparallel with the South Carpathians fold and thrust belt (Fig. 1)43. The associated folding during the Walachian compressional stage of Pleistocene age44 is thought to play an ...
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