First results from the CROP- 11 deep seismic profile, central Apennines, Italy: evidence of mid-crustal folding (Articolo in rivista)

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  • First results from the CROP- 11 deep seismic profile, central Apennines, Italy: evidence of mid-crustal folding (Articolo in rivista) (literal)
Anno
  • 2006-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1144/0016-764920-002 (literal)
Alternative label
  • BILLI A.* , TIBERTI, M. M**, CAVINATO, GP***, COSENTINO D.*, DI LUZIO E***, KELLER JVA****, KLUTH C*****, ORLANDO L******, PAROTTO M*, PRATURLON A*, ROMANELLI M*******, STORTI F*, WARDELL N*******. (2006)
    First results from the CROP- 11 deep seismic profile, central Apennines, Italy: evidence of mid-crustal folding
    in Journal of the Geological Society (Lond.)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • BILLI A.* , TIBERTI, M. M**, CAVINATO, GP***, COSENTINO D.*, DI LUZIO E***, KELLER JVA****, KLUTH C*****, ORLANDO L******, PAROTTO M*, PRATURLON A*, ROMANELLI M*******, STORTI F*, WARDELL N*******. (literal)
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  • 163 (literal)
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  • 4 (literal)
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  • 4 (literal)
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  • Scopu (literal)
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  • * Dipartimento di Scienze Geologiche, Universita` 'Roma Tre', **Istituto Nazionale di Geofisica e Vulcanologia, 00143, Rome, Italy *** CNR-IGAG **** ChevronTexaco Energy Technology Co., San Ramon, CA, 94583, USA ***** Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO 80401, USA, ******Dipartimento di Idraulica, Trasporti e Strade, Universita`'La Sapienza', 00184 Rome, Italy *******Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, 34010 Trieste, Italy (literal)
Titolo
  • First results from the CROP- 11 deep seismic profile, central Apennines, Italy: evidence of mid-crustal folding (literal)
Abstract
  • The CROP-11 deep seismic profile across the central Apennines, Italy, reveals a previously unknown, mid-crustal antiform here interpreted as a fault-bend fold-like structure. The seismic facies and gravity signature suggest that this structure consists of low-grade metamorphic rocks. Geomorphological, stratigraphic and tectonic evidence in the overlying shallow thrusts suggests that this structure developed in early to mid- Messinian time and grew out of sequence in late Messinian-Pliocene time. The out-of-sequence growth may reflect a taper subcriticality stage of the Apenninic thrust wedge, which induced renewed contraction in the rear. (literal)
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