http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28369
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. 1, Tiberti M.M. 2, Cavinato G.P 3., Cosentino D. 1, Di Luzio E. 3, Keller J.V.A. 4, Kluth C.5, Orlando L. 6, Parotto M. 1, Praturlon A. 1, Romanelli M. 7, Storti F.1, Wardell N. 7 (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. 1, Tiberti M.M. 2, Cavinato G.P 3., Cosentino D. 1, Di Luzio E. 3, Keller J.V.A. 4, Kluth C.5, Orlando L. 6, Parotto M. 1, Praturlon A. 1, Romanelli M. 7, Storti F.1, Wardell N. 7 (literal)
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- http://jgs.geoscienceworld.org/content/163/4/583.abstract (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
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- ISI Web of Science (WOS) (literal)
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- 1. Univ Roma Tre, Dipartimento Sci Geol, I-00146 Rome, Italy
2. Ist Nazl Geofis & Vulcanol, I-00143 Rome, Italy
3. CNR, Ist Geol Ambientale & Geoingn, I-00185 Rome, Italy
4. ChevronTexaco Energy Technol Co, San Ramon, CA 94583 USA
5. Colorado Sch Mines, Dept Geol & Geol Engn, Golden, CO 80401 USA
6. Univ Roma La Sapienza, Dipartimento Idraulica Trasporti & Strade, I-00184 Rome, Italy
7. Ist Nazl Oceanog & Geofis, I-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 suberiticality stage of the Apenninic thrust wedge, which induced renewed contraction in the rear. (literal)
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