1. Studi Geologici Camerti
  2. 2 - Studi Geologici Camerti - Volume Speciale
  3. 2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002
Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1310
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Campo DCValoreLingua
dc.contributor.authorGALINDO-ZALDIVAR, J.-
dc.contributor.authorGIL, A.J.-
dc.contributor.authorBORQUE, M.J.-
dc.contributor.authorMARIN-LECHADO, C.-
dc.contributor.authorRUANO, P.-
dc.contributor.authorSANZ DE GALDEANO, C.-
dc.date.accessioned2017-12-04T10:29:39Z-
dc.date.available2017-12-04T10:29:39Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 63-66it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/677-
dc.description.abstractTue internal zones of the Betic Cordilleras are deformed since Middle Miocene by k:ilometre-sized E-W oriented folds coeval with fault development. Faults are generally normal in the central trans­ect. The Zafarraya Fault, responsible for the 1884 Andalucfa Earthquak:e, is located at the northem limb of the Sierra Tejeda anti­form, and could be interpreted as a collapse structure developed along the extemal arch of the uplifted fold. Tue set up of a GPS net­work in the Sierra Tejeda will allow us to study the present-day deformation relationships of folds and faults in the area.en
dc.publisherUniversità di Camerinoit
dc.subjectBetic Cordilleras - Zafarraya Fault - Sierra Tejeda antiform - GPS networken
dc.titleTHE ZAFARRAYA FAULT IN THE FRAME OF THE ACTIVE TECTONIC STRUCTURES OF THE CENTRAL BETIC CORDILLERA (SOUTHERN SPAIN)en
dc.description.pages63-66-
E' visualizzato nelle collezioni:2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002

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