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Low angle normal faulting and focused exhumation associated with late Pliocene change in tectonic style in the southern Apennines (Italy)

Author:
Mazzoli, Stefano - Ascione, Alessandra - Buscher, Jamie T. - Pignalosa, Antonio - Valente, Ettore - Zattin, Massimiliano
Publisher:
American Geophysical Union
Year
: 2014
DOI: 10.1002/2014TC003608
URI: https://libsearch.um.ac.ir:443/fum/handle/fum/843893
Keyword(s): extensional tectonics,low,exhumation,uplift,tectonic geomorphology,fold and thrust belts,1140 Thermochronology,8036 Paleoseismology,8109 Continental tectonics: extensional,8175 Tectonics and landscape evolution,8102 Continental contractional orogenic belts and inversion tectonics
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    Low angle normal faulting and focused exhumation associated with late Pliocene change in tectonic style in the southern Apennines (Italy)

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date accessioned2020-03-12T11:00:58Z
date available2020-03-12T11:00:58Z
date issued2014
identifier issn0278-7407
identifier other10.1002-2014TC003608.pdf
identifier urihttps://libsearch.um.ac.ir:443/fum/handle/fum/843893
formatgeneral
languageEnglish
publisherAmerican Geophysical Union
titleLow angle normal faulting and focused exhumation associated with late Pliocene change in tectonic style in the southern Apennines (Italy)
typeJournal Paper
contenttypeMetadata Only
identifier padid6670346
subject keywordsextensional tectonics
subject keywordslow
subject keywordsexhumation
subject keywordsuplift
subject keywordstectonic geomorphology
subject keywordsfold and thrust belts
subject keywords1140 Thermochronology
subject keywords8036 Paleoseismology
subject keywords8109 Continental tectonics: extensional
subject keywords8175 Tectonics and landscape evolution
subject keywords8102 Continental contractional orogenic belts and inversion tectonics
identifier doi10.1002/2014TC003608
journal titleTectonics
journal volume33
journal issue9
filesize5117916
citations0
contributor rawauthorMazzoli, Stefano - Ascione, Alessandra - Buscher, Jamie T. - Pignalosa, Antonio - Valente, Ettore - Zattin, Massimiliano
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