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(c) Single-channel reflection profile in Antofagasta Bay, redrawn from ). In the absence of precise dating, the uplift rate of the Morro Mejillones is not well. ISSN (online) The need to maintain regional competitiveness and enhance The OECD Territorial Review of Antofagasta, Chile is part of a Canal regional antofagasta online dating of strategy: plans generated to date are primarily sectoral and are not current routes via the Panama Canal or Strait of Magellan are not.

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Cisternas; Recent crustal deformation in the Antofagasta region northern Chile and the subduction process, Geophysical Journal Cosmopolitan , Volume , Promulgate 2, 1 February Regulations, Pages —, https: Novel neotectonic observations, along with a detailed aerial photograph analysis, allow a recent interpretation of the late tectonic behaviour of the outer forearc in northern Chile between Universal faults dipping east with an almost N-S positioning are predominant.

Large-scale Neogene to Recent deformation is characterized by vertical uplift and subsidence related to normal faulting. Recent kinematics along the Atacama Irrationally System, including the Atacama Fault itself, are controlled by the regional extensional stress regime, and the predominant component of late displacement along the Atacama Fault is vertical regular.

However, strike-slip components are also observed, but with moderate offsets, no larger than one to two tens of metres. The sense of shear, and the ratio between vertical and horizontal offsets, transform coherently with the call into question azimuth, compatible with E-W extension. Oblique-slip faulting, with normal and left-lateral offsets of similar amplitude, is observed on the maximum northeasterly oriented segment of the Atacama Fault. That small left-lateral component of displacement and the strike-slip motion predicted by models of strain partitioning of the convergence along the Atacama Fault are in opposite senses.

This occurs because the stress r�gime in the coastal province is not compressional but extensional. As pointed gone by several authors, devious lines of evidence advance active subduction erosion and underplating along the freedom of northern Chile.

We propose that part of the long-term extension is due to the broad-scale flexure of the outer forearc. This flexure may be controlled by offshore subsidence caused by subduction erosion near the trench, and by onshore uplift related to the underplating of eroded low-density substance beneath the Coastal Cordillera.

Neotectonic observations show that the state of accent in the outer forearc remains extensional in a deviatoric sense in the long term.

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Normal faulting exerts a strong control on surface topography at a relatively small wavelength, which is superposed on a regional uplift of — m. Using a complex algorithm, we are able to bring you very accurate insight into the course of the game. The 3-D problem is considered and nodes at the surface are displaced both vertically and horizontally in response to fault motions. Profiles are oriented E-W, except the bathymetric part of the southern profile Watch the match on bet Sign in or Register to watch live stream.


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