Morphology and geology of the continental shelf and upper slope of southern Central Chile (33°S–43°S)

The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30 years. This work summarizes the geologic setting of the southern Central Chilean Continental shelf (33°S–43°S) using recently published geop...

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Published in	International journal of earth sciences : Geologische Rundschau Vol. 103; no. 7; pp. 1765 - 1787
Main Authors	Völker, David, Geersen, Jacob, Contreras-Reyes, Eduardo, Sellanes, Javier, Pantoja, Silvio, Rabbel, Wolfgang, Thorwart, Martin, Reichert, Christian, Block, Martin, Weinrebe, Wilhelm Reimer
Format	Journal Article
Language	English
Published	Berlin/Heidelberg Springer Berlin Heidelberg 01.10.2014 Springer Nature B.V
Subjects	Bathymetry Biota Bottom currents Continental crust Continental margins Continental shelves Continental slope Earth and Environmental Science Earth Sciences Geochemistry Geology Geophysics/Geodesy Mineral Resources Morphology Oligocene Original Paper Quaternary Sedimentology Slope stability Structural Geology Submarine canyons Upwelling Chile Shelf basins Submarine faults Shelf sedimentation Fluid seepage Southern Central Chile Bathymetry Seismicity
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Abstract	The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30 years. This work summarizes the geologic setting of the southern Central Chilean Continental shelf (33°S–43°S) using recently published geophysical, seismological, sedimentological and bio-geochemical data. Additionally, unpublished data such as reflection seismic profiles, swath bathymetry and observations on biota that allow further insights into the evolution of this continental platform are integrated. The outcome is an overview of the current knowledge about the geology of the southern Central Chilean shelf and upper slope. We observe both patches of reduced as well as high recent sedimentation on the shelf and upper slope, due to local redistribution of fluvial input, mainly governed by bottom currents and submarine canyons and highly productive upwelling zones. Shelf basins show highly variable thickness of Oligocene-Quaternary sedimentary units that are dissected by the marine continuations of upper plate faults known from land. Seismic velocity studies indicate that a paleo-accretionary complex that is sandwiched between the present, relatively small active accretionary prism and the continental crust forms the bulk of the continental margin of southern Central Chile.
AbstractList	The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30 years. This work summarizes the geologic setting of the southern Central Chilean Continental shelf (33 degree S-43 degree S) using recently published geophysical, seismological, sedimentological and bio-geochemical data. Additionally, unpublished data such as reflection seismic profiles, swath bathymetry and observations on biota that allow further insights into the evolution of this continental platform are integrated. The outcome is an overview of the current knowledge about the geology of the southern Central Chilean shelf and upper slope. We observe both patches of reduced as well as high recent sedimentation on the shelf and upper slope, due to local redistribution of fluvial input, mainly governed by bottom currents and submarine canyons and highly productive upwelling zones. Shelf basins show highly variable thickness of Oligocene-Quaternary sedimentary units that are dissected by the marine continuations of upper plate faults known from land. Seismic velocity studies indicate that a paleo-accretionary complex that is sandwiched between the present, relatively small active accretionary prism and the continental crust forms the bulk of the continental margin of southern Central Chile. The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30 years. This work summarizes the geologic setting of the southern Central Chilean Continental shelf (33°S–43°S) using recently published geophysical, seismological, sedimentological and bio-geochemical data. Additionally, unpublished data such as reflection seismic profiles, swath bathymetry and observations on biota that allow further insights into the evolution of this continental platform are integrated. The outcome is an overview of the current knowledge about the geology of the southern Central Chilean shelf and upper slope. We observe both patches of reduced as well as high recent sedimentation on the shelf and upper slope, due to local redistribution of fluvial input, mainly governed by bottom currents and submarine canyons and highly productive upwelling zones. Shelf basins show highly variable thickness of Oligocene-Quaternary sedimentary units that are dissected by the marine continuations of upper plate faults known from land. Seismic velocity studies indicate that a paleo-accretionary complex that is sandwiched between the present, relatively small active accretionary prism and the continental crust forms the bulk of the continental margin of southern Central Chile. Issue Title: Volatiles and Fluids in Subduction Zones The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30 years. This work summarizes the geologic setting of the southern Central Chilean Continental shelf (33°S-43°S) using recently published geophysical, seismological, sedimentological and bio-geochemical data. Additionally, unpublished data such as reflection seismic profiles, swath bathymetry and observations on biota that allow further insights into the evolution of this continental platform are integrated. The outcome is an overview of the current knowledge about the geology of the southern Central Chilean shelf and upper slope. We observe both patches of reduced as well as high recent sedimentation on the shelf and upper slope, due to local redistribution of fluvial input, mainly governed by bottom currents and submarine canyons and highly productive upwelling zones. Shelf basins show highly variable thickness of Oligocene-Quaternary sedimentary units that are dissected by the marine continuations of upper plate faults known from land. Seismic velocity studies indicate that a paleo-accretionary complex that is sandwiched between the present, relatively small active accretionary prism and the continental crust forms the bulk of the continental margin of southern Central Chile.[PUBLICATION ABSTRACT]
Author	Thorwart, Martin Völker, David Weinrebe, Wilhelm Reimer Contreras-Reyes, Eduardo Rabbel, Wolfgang Geersen, Jacob Sellanes, Javier Pantoja, Silvio Reichert, Christian Block, Martin
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Snippet	The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last... Issue Title: Volatiles and Fluids in Subduction Zones The continental shelf and slope of southern Central Chile have been subject to a number of international... The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30...
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StartPage	1765
SubjectTerms	Bathymetry Biota Bottom currents Continental crust Continental margins Continental shelves Continental slope Earth and Environmental Science Earth Sciences Geochemistry Geology Geophysics/Geodesy Mineral Resources Morphology Oligocene Original Paper Quaternary Sedimentology Slope stability Structural Geology Submarine canyons Upwelling
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Title	Morphology and geology of the continental shelf and upper slope of southern Central Chile (33°S–43°S)
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