Extensional basins in the tectonically bimodal central Apennines fold-thrust belt, Italy: response to corner flow above a subducting slab in retrograde motion. (Articolo in rivista)

Type

• Articolo in rivista (Classe)
• Prodotto della ricerca (Classe)

Label

• Extensional basins in the tectonically bimodal central Apennines fold-thrust belt, Italy: response to corner flow above a subducting slab in retrograde motion. (Articolo in rivista) (literal)

Anno

• 1999-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1130/0091-7613 (literal)

Alternative label

• CAVINATO G. P. & DE CELLES P. (1999)
  Extensional basins in the tectonically bimodal central Apennines fold-thrust belt, Italy: response to corner flow above a subducting slab in retrograde motion.
  in Geology (Boulder Colo., Online); Geological Society Of America, Inc., Boulder (Stati Uniti d'America)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• CAVINATO G. P. & DE CELLES P. (literal)

Pagina inizio

• 955 (literal)

Pagina fine

• 958 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 27 (literal)

Rivista

• Geology (Rivista)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali

• 4 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo

• 10 (literal)

Note

• ISI Web of Science (WOS) (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• CNR- IGAG (literal)

Titolo

• Extensional basins in the tectonically bimodal central Apennines fold-thrust belt, Italy: response to corner flow above a subducting slab in retrograde motion. (literal)

Abstract

• The Apennines fold-thrust belt has developed over the past ~20 m.y. in response to southeastward retrograde migration of the Adriatic trench in a region of ongoing subduction but little plate convergence. The orogenic belt is characterized by a gently sloping southwestern flank in a state of regional extensional collapse, and a steeply sloping northeastern flank in regional contraction. In any given area in the central Apennines, the chronologies of thrusting and subsequent extension provide an estimate of the time required for attainment of high elevation (2.5-3.0 km). The time between initial extension and eruption of local ultramafic lavas provides an estimate of the time required to collapse by regional crustal thinning. These estimates suggest that the northeastern, contractional flank of the range is rising at least twice as fast as the southwestern flank is collapsing. We propose that the bimodal state of stress in the Apennines is maintained by corner flow in the mantle wedge beneath the crest of the range. (literal)

Editore

• Geological Society Of America, Inc. (Editore)

Prodotto di

• Geologia del Quaternario, valutazioni di pericolosità geologica, sottosuolo di aree urbane. (TA.P05.025.003) (Modulo)
• Struttura crostale ed evoluzione geodinamica dell'area mediterranea (TA.P05.025.008) (Modulo)
• Institute of environmental geology and geoengineering (IGAG) (Istituto)

Autore CNR

• GIAN PAOLO CAVINATO (Persona)

Incoming links:

Prodotto

• Institute of environmental geology and geoengineering (IGAG) (Istituto)
• Geologia del Quaternario, valutazioni di pericolosità geologica, sottosuolo di aree urbane. (TA.P05.025.003) (Modulo)
• Struttura crostale ed evoluzione geodinamica dell'area mediterranea (TA.P05.025.008) (Modulo)

Autore CNR di

• GIAN PAOLO CAVINATO (Persona)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Geology (Rivista)

Editore di

• Geological Society Of America, Inc. (Editore)