Active tectonics of the North Chilean marine forearc and adjacent oceanic Nazca Plate.

Geersen, Jacob , Ranero, César R., Klaucke, Ingo , Behrmann, Jan H. , Kopp, Heidrun , Tréhu, Anne M., Contreras-Reyes, Eduardo, Barckhausen, Udo and Reichert, Christian (2018) Active tectonics of the North Chilean marine forearc and adjacent oceanic Nazca Plate. Open Access Tectonics, 37 (11). pp. 4194-4211. DOI 10.1029/2018TC005087.

[img]
Preview
Text (Accepted manuscript)
10.1029_2018TC005087.pdf - Accepted Version

Download (13Mb) | Preview
[img] Text
Geersen_et_al-2018-Tectonics.pdf - Published Version
Restricted to Registered users only

Download (13Mb) | Contact

Supplementary data:

Abstract

Key Points:

Multibeam bathymetric and seismic reflection data image the structure of the North Chilean marine forearc and the oceanic Nazca plate

The structural character and tectonic configuration of the offshore forearc and the oceanic plate change significantly along the margin

The derived pattern of permanent deformation may hold information for studying seismicity or other types of short term deformation

New multibeam bathymetry allows an unprecedented view of the tectonic regime and its along‐strike heterogeneity of the North Chilean marine forearc and the oceanic Nazca Plate between 19‐22.75°S. Combining bathymetric and backscatter information from the multibeam data with sub‐bottom profiler and published and previously unpublished legacy seismic reflection lines, we derive a tectonic map. The new map reveals a middle and upper‐slope configuration dominated by pervasive extensional faulting, with some faults outlining a >500 km long ridge that may represent the remnants of a Jurassic or pre‐Jurassic magmatic arc. Lower slope deformation is more variable and includes slope‐failures, normal faulting, re‐entrant embayments, and NW‐SE trending anticlines and synclines. This complex pattern likely results from the combination of subducting lower‐plate topography, gravitational forearc collapse, and the accumulation of permanent deformation over multiple earthquake cycles. We find little evidence for widespread fluid seepage despite a highly faulted upper‐plate. An explanation could be a lack of fluid sources due to the sediment starved nature of the trench and most of the upper‐plate in vicinity of the hyper‐arid Atacama Desert. Changes in forearc architecture partly correlate to structural variations of the oceanic Nazca Plate, which is dominated by the spreading‐related abyssal hill fabric and is regionally overprinted by the Iquique Ridge. The ridge collides with the forearc around 20‐21°S. South of the ridge‐forearc intersection, bending‐related horst‐and‐grabens result in vertical seafloor offsets of hundreds of meters. To the north, plate‐bending is accommodated by reactivation of the paleo‐spreading fabric and new horst‐and‐grabens do not develop.

Document Type: Article
Keywords: Permanent deformation, subduction-zone, active tectonics, North Chile, Marine seismics, Multibeam bathymetry
Research affiliation: OceanRep > The Future Ocean - Cluster of Excellence
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1029/2018TC005087
ISSN: 0278-7407
Projects: Future Ocean, FONDECYT
Expeditions/Models/Experiments:
Date Deposited: 16 Oct 2018 07:53
Last Modified: 14 Apr 2019 23:38
URI: http://oceanrep.geomar.de/id/eprint/44496

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...