A recent phase of accretion along the southern Costa Rican subduction zone

12 pages, 9 figures

Saved in:
Bibliographic Details
Main Authors: Bangs, Nathan L., McIntosh, Kirk D., Silver, Eli A., Kluesner, Jared W., Ranero, César R.
Other Authors: National Science Foundation (US)
Format: artículo biblioteca
Published: Elsevier 2016-06
Subjects:Subduction accretion, Tectonic erosion, Costa Rican subduction zone, 3D seismic imaging, Accretionary wedge deformation,
Online Access:http://hdl.handle.net/10261/133324
http://dx.doi.org/10.13039/100000001
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-icm-es-10261-133324
record_format koha
spelling dig-icm-es-10261-1333242020-03-04T02:00:31Z A recent phase of accretion along the southern Costa Rican subduction zone Bangs, Nathan L. McIntosh, Kirk D. Silver, Eli A. Kluesner, Jared W. Ranero, César R. National Science Foundation (US) Subduction accretion Tectonic erosion Costa Rican subduction zone 3D seismic imaging Accretionary wedge deformation 12 pages, 9 figures In 2011 we acquired a 3D seismic reflection volume across the Costa Rica margin NW of the Osa Peninsula to investigate the complex structure and the development of the seismogenic zone within the Costa Rican subduction zone in the vicinity of recent International Ocean Drilling Program (IODP) drilling. In contrast to previous interpretations, these newly acquired seismic images show that the margin wedge is composed of a layered fabric that is consistent with clastic sediments, similar to materials recovered from IODP drilling, that have been thrust and thickened into thrust-bounded folded sequences. These structures are consistent with a balanced sequence that has been frontally accreted in the context of an accretionary model. We interpret these sequences as sediment originally deposited on the subducting crust in a trench basin created by the southward migration of the Cocos-Nazca-Caribbean triple junction, and accreted during recent margin subduction that also accelerated with passage of the triple junction. The margin is composed of relatively rapidly accreted sediment that was added to the margin during a phase of accretion within the last ~5 Ma that was probably preceded throughout the Neogene by periods of non-accretion or erosion This work was supported by National Science Foundation Grant numbers 1435386 and 0851380 Peer Reviewed 2016-06-10T11:47:25Z 2016-06-10T11:47:25Z 2016-06 2016-06-10T11:47:25Z artículo http://purl.org/coar/resource_type/c_6501 doi: 10.1016/j.epsl.2016.03.008 issn: 0012-821X Earth and Planetary Science Letters 443: 204-215 (2016) http://hdl.handle.net/10261/133324 10.1016/j.epsl.2016.03.008 http://dx.doi.org/10.13039/100000001 https://dx.doi.org/10.1016/j.epsl.2016.03.008 Sí open Elsevier
institution ICM ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-icm-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del ICM España
topic Subduction accretion
Tectonic erosion
Costa Rican subduction zone
3D seismic imaging
Accretionary wedge deformation
Subduction accretion
Tectonic erosion
Costa Rican subduction zone
3D seismic imaging
Accretionary wedge deformation
spellingShingle Subduction accretion
Tectonic erosion
Costa Rican subduction zone
3D seismic imaging
Accretionary wedge deformation
Subduction accretion
Tectonic erosion
Costa Rican subduction zone
3D seismic imaging
Accretionary wedge deformation
Bangs, Nathan L.
McIntosh, Kirk D.
Silver, Eli A.
Kluesner, Jared W.
Ranero, César R.
A recent phase of accretion along the southern Costa Rican subduction zone
description 12 pages, 9 figures
author2 National Science Foundation (US)
author_facet National Science Foundation (US)
Bangs, Nathan L.
McIntosh, Kirk D.
Silver, Eli A.
Kluesner, Jared W.
Ranero, César R.
format artículo
topic_facet Subduction accretion
Tectonic erosion
Costa Rican subduction zone
3D seismic imaging
Accretionary wedge deformation
author Bangs, Nathan L.
McIntosh, Kirk D.
Silver, Eli A.
Kluesner, Jared W.
Ranero, César R.
author_sort Bangs, Nathan L.
title A recent phase of accretion along the southern Costa Rican subduction zone
title_short A recent phase of accretion along the southern Costa Rican subduction zone
title_full A recent phase of accretion along the southern Costa Rican subduction zone
title_fullStr A recent phase of accretion along the southern Costa Rican subduction zone
title_full_unstemmed A recent phase of accretion along the southern Costa Rican subduction zone
title_sort recent phase of accretion along the southern costa rican subduction zone
publisher Elsevier
publishDate 2016-06
url http://hdl.handle.net/10261/133324
http://dx.doi.org/10.13039/100000001
work_keys_str_mv AT bangsnathanl arecentphaseofaccretionalongthesoutherncostaricansubductionzone
AT mcintoshkirkd arecentphaseofaccretionalongthesoutherncostaricansubductionzone
AT silverelia arecentphaseofaccretionalongthesoutherncostaricansubductionzone
AT kluesnerjaredw arecentphaseofaccretionalongthesoutherncostaricansubductionzone
AT ranerocesarr arecentphaseofaccretionalongthesoutherncostaricansubductionzone
AT bangsnathanl recentphaseofaccretionalongthesoutherncostaricansubductionzone
AT mcintoshkirkd recentphaseofaccretionalongthesoutherncostaricansubductionzone
AT silverelia recentphaseofaccretionalongthesoutherncostaricansubductionzone
AT kluesnerjaredw recentphaseofaccretionalongthesoutherncostaricansubductionzone
AT ranerocesarr recentphaseofaccretionalongthesoutherncostaricansubductionzone
_version_ 1777666428906766336