Results 71 to 80 of about 22,020,665 (180)
In extensional continental settings, crustal-scale normal faults can accommodate deformation and subsidence at their hanging wall via activation and deactivation of subsidiary tectonic structures.
Gianluca Vignaroli +12 more
doaj +1 more source
Paleostress analysis as a key to margin extension: The Penghu Islands, South China Sea [PDF]
Abstract The Penghu Islands belong to the Eurasian passive margin, west of the collision zone of Taiwan. From south to north, the South China Sea basins become narrower and disappear in the Taiwan Strait area. The presence of the Penghu Islands allow description of the tectonic evolution of the margin through the reconstruction of tectonic ...
Angelier, Jacques +4 more
openaire +1 more source
Contemporaneous Stress in Taiwan: Evidence for Orogen‐Parallel Extension and Lower Crustal Extrusion
Abstract Syn‐to late‐orogenic extension caused by gravitational collapse is a process that has been documented in most orogens. In this paper, we investigate the contemporaneous stress field in Taiwan to examine syn‐orogenic extensional faulting and the possible gravitational collapse modes by which it is taking place.
O. Lozano‐Blanco +5 more
wiley +1 more source
Abstract The fragmentation of continents results in microplates that rotate to accommodate the lateral propagation of bounding rifts. Yet, the relationships between microplate rotation rates, fault slip, and kinematics at propagating rift tips remain unknown.
Asenath Kwagalakwe +15 more
wiley +1 more source
Morphometric Evidence for Cenozoic Intraplate Reactivation in NW Uruguay
Abstract Located in eastern South America, Uruguay has been considered tectonically inactive since rifting in the Late Cretaceous. Here, we use a high‐resolution digital elevation model and field observations to investigate the presence of recent tectonic activity in the Basaltic Plateau, northwest Uruguay.
Mauricio B. Haag +5 more
wiley +1 more source
Paleostress field reconstruction and revised tectonic history of the Donbas fold and thrust belt (Ukraine and Russia). [PDF]
In the WNW-ESE Donbas fold belt (DF), inversion of 3500 microtectonic data collected at 135 sites, in Proterozoic, Devonian, Carboniferous, and Cretaceous competent rocks allowed reconstruction of 123 local stress states.
Stephenson, R.A. +4 more
core +2 more sources
y-gRaph: An OpenOffice application to reconstruct paleostress fields from striated faults
An application (y-gRaph) to reconstruct paleostress fields from faults striations by means of the y–R diagram method is here presented. Based on modified Bott´s equation, the diagram relates y (azimuth of the maximum horizontal stress axis) and R (stress
Calvín, P
core +2 more sources
Abstract Sant'Anna Pelago is located near the extensional front of the Northern Apennines (Italy) between Modena and Lucca, an area characterized by multiple lateral steps of the NW‐SE striking tectonic system and orographic divide. The region is affected by significant instrumental seismicity with over a thousand recorded events (0.5 < M < 4.8) from ...
S. Lenci +5 more
wiley +1 more source
Active Deformation and Paleostress Analysis in the Pakua Anticline Area of Western Taiwan
This paper presents a review of strain-stress relationships in the activeTaiwan collision at different scales based on numerical modeling.As thedigital computer has become an important research tool due to its capabilityof performing numerical simulations of real tectonic processes,a massof accurate and comprehensive database is required to assure the ...
Jian-Cheng Lee +5 more
openaire +1 more source
Abstract This study presents the first rigorous statistical analysis of the present‐day crustal stress along the western margin of the North American Plate, covering the entire Canadian Cordillera and Alaska. Using circular statistics and geometric tests, we develop a regional stress province model that constrains the directions of first‐order stresses.
T. Stephan, E. Enkelmann
wiley +1 more source

