Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/7896
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Guarnieri, P.; Univ. di Catania | en |
dc.contributor.authorall | Vinciguerra, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.date.accessioned | 2012-03-19T08:57:30Z | en |
dc.date.available | 2012-03-19T08:57:30Z | en |
dc.date.issued | 2004 | en |
dc.identifier.uri | http://hdl.handle.net/2122/7896 | en |
dc.description.abstract | A Neogene transcurrent fault system a ecting the Apenninic-Maghrebian thrust belt, located in northwestern Sicily, has been investigated using fractal analysis. The present-day structural setting of the sector between the Palermo and Madonie Mountains is the result of the superim- position, in space and time, of two distinct deformational events, a Miocene southeast-verging thrusting followed by Messinian to Pliocene strike-slip faulting, which cuts obliquely through the compressive fronts. The spatial distribution properties of the fault array were investigated by means of a fractal analysis. Fractal dimension was computed by adopting the correlation integral method. Fractal ranges have been evidenced between 350 and 3000 m. The fractal di- mension obtained for the whole array is D = 1:66. The scaling spatial distribution property of the fault array has been analyzed by calculating the fractal dimension with a moving window | en |
dc.language.iso | English | en |
dc.publisher.name | World Scientific Publishing Company | en |
dc.relation.ispartof | Fractals | en |
dc.relation.ispartofseries | 1/12 (2004) | en |
dc.subject | Fractal Properties; Correlation Integral; Transcurrent Faults; Sicily | en |
dc.title | FRACTAL PROPERTIES OF A NEOGENE FAULT SYSTEM IN NORTHWESTERN SICILY, ITALY | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 41-48 | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.09. Structural geology | en |
dc.description.obiettivoSpecifico | 3.2. Tettonica attiva | en |
dc.description.journalType | N/A or not JCR | en |
dc.description.fulltext | restricted | en |
dc.relation.issn | 0218-348X | en |
dc.relation.eissn | 1793-6543 | en |
dc.contributor.author | Guarnieri, P. | en |
dc.contributor.author | Vinciguerra, S. | en |
dc.contributor.department | Univ. di Catania | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Dipartimento di Scienze Geologiche, Università degli Studi di Catania, Italy | - |
crisitem.author.orcid | 0000-0002-6939-3549 | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
Files in This Item:
File | Description | Size | Format | Existing users please Login |
---|---|---|---|---|
Guarnieri_Fractals_2004.pdf | 3.79 MB | Adobe PDF |
Page view(s)
97
checked on Apr 24, 2024
Download(s)
16
checked on Apr 24, 2024