Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)

The so-called MarratxiAnticline, which separates the Quaternary basins oflnca and Palma Bay (Mallorca Island), does not correspond to a true compressive feature. It only represents an NNW-SSE trending antiform resulting from the adaptation, and subsequent dissection, of Quaternary gently-dipping eol...

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Detalhes bibliográficos
Autores: Silva, P. G., González Hernández, F. M., Goy, José L., Zazo, C.
Formato: artículo
Fecha de publicación:1997
País:España
Recursos:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/10462
Acesso em linha:http://hdl.handle.net/10272/10462
Access Level:acceso abierto
Palavra-chave:Neotectonics
Rollover monoclinal folding
Drainage
Plio-Quaternary
Mallorca
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spelling Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)Origin and Dissection of the Plio-Quaternary Marratxí Antiform (Mallorca Island, Spain)Silva, P. G.González Hernández, F. M.Goy, José L.Zazo, C.NeotectonicsRollover monoclinal foldingDrainagePlio-QuaternaryMallorcaThe so-called MarratxiAnticline, which separates the Quaternary basins oflnca and Palma Bay (Mallorca Island), does not correspond to a true compressive feature. It only represents an NNW-SSE trending antiform resulting from the adaptation, and subsequent dissection, of Quaternary gently-dipping eolian sedimentation of calcarenitic nature coming from the Palma Bay (South limb), to a previous horst-type structural high constituted by structured mesozoic, paleogene and early miocene materials topped by sub-horizontal upper Pliocene littoral calcarenites. These last also constitutes the moderate to strongly-dipping calcarenitic cuestas of the northern limb of the antiform. Its structuration can be explained in terms of Plio-Quaternary surficial monoclinal folding, probably linked to rollover-type processes along previous lateral ramps generated during the early Miocene nappe emplacement phase along the northern border of the mentioned structural-high. Topographic disruption promoted by this structure gave place to Quaternary defeating of the drainage coming from the Sierra de Tramuntana to the Palma Bay. Subsequent late Pleistocene headward erosion along the ses Mates creek, probably linked to the Last Glacial sea-level drop, lead the generation of the presently transverse drainageSociedad Geológica de España19971997-01-0119971997-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/10462reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/104622026-06-02T14:58:11Z
dc.title.none.fl_str_mv Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
Origin and Dissection of the Plio-Quaternary Marratxí Antiform (Mallorca Island, Spain)
title Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
spellingShingle Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
Silva, P. G.
Neotectonics
Rollover monoclinal folding
Drainage
Plio-Quaternary
Mallorca
title_short Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
title_full Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
title_fullStr Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
title_full_unstemmed Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
title_sort Origen y desmantelamiento del Antiforme Plio-Cuaternario de Marratxí (Mallorca, España)
dc.creator.none.fl_str_mv Silva, P. G.
González Hernández, F. M.
Goy, José L.
Zazo, C.
author Silva, P. G.
author_facet Silva, P. G.
González Hernández, F. M.
Goy, José L.
Zazo, C.
author_role author
author2 González Hernández, F. M.
Goy, José L.
Zazo, C.
author2_role author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Neotectonics
Rollover monoclinal folding
Drainage
Plio-Quaternary
Mallorca
topic Neotectonics
Rollover monoclinal folding
Drainage
Plio-Quaternary
Mallorca
description The so-called MarratxiAnticline, which separates the Quaternary basins oflnca and Palma Bay (Mallorca Island), does not correspond to a true compressive feature. It only represents an NNW-SSE trending antiform resulting from the adaptation, and subsequent dissection, of Quaternary gently-dipping eolian sedimentation of calcarenitic nature coming from the Palma Bay (South limb), to a previous horst-type structural high constituted by structured mesozoic, paleogene and early miocene materials topped by sub-horizontal upper Pliocene littoral calcarenites. These last also constitutes the moderate to strongly-dipping calcarenitic cuestas of the northern limb of the antiform. Its structuration can be explained in terms of Plio-Quaternary surficial monoclinal folding, probably linked to rollover-type processes along previous lateral ramps generated during the early Miocene nappe emplacement phase along the northern border of the mentioned structural-high. Topographic disruption promoted by this structure gave place to Quaternary defeating of the drainage coming from the Sierra de Tramuntana to the Palma Bay. Subsequent late Pleistocene headward erosion along the ses Mates creek, probably linked to the Last Glacial sea-level drop, lead the generation of the presently transverse drainage
publishDate 1997
dc.date.none.fl_str_mv 1997
1997-01-01
1997
1997-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/10462
url http://hdl.handle.net/10272/10462
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
dc.source.none.fl_str_mv reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,811543

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