http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28683
Studying travertines for neotectonics investigations: MiddleLate Pleistocene syn-tectonic travertine deposition at Serre di Rapolano (Northern Apennines, Italy) (Articolo in rivista)
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- Studying travertines for neotectonics investigations: MiddleLate Pleistocene syn-tectonic travertine deposition at Serre di Rapolano (Northern Apennines, Italy) (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00531-009-0456-y (literal)
- Alternative label
Brogi A., Capezzuoli E., Aqué R., Branca M. E., Voltaggio M. (2010)
Studying travertines for neotectonics investigations: MiddleLate Pleistocene syn-tectonic travertine deposition at Serre di Rapolano (Northern Apennines, Italy)
in International journal of earth sciences (1999, Print)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Brogi A., Capezzuoli E., Aqué R., Branca M. E., Voltaggio M. (literal)
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- http://www.springerlink.com/content/n103298137353x31/ (literal)
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- Rivista
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- DOI: 10.1007/s00531-009-0456-y (literal)
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- Brogi A:Dipartimento di Scienze della Terra, Universita` di Siena;
E. Capezzuoli: Dipartimento di Scienze della Terra, Universita` di Siena;
R. Aque´:Dipartimento di Scienze della Terra, Universita` di Siena;
Branca M: Istituto di Geologia Ambientale e geoingegneria, CNR , Roma;
Voltaggio M.Istituto di Geologia Ambientale e geoingegneria, CNR , Roma (literal)
- Titolo
- Studying travertines for neotectonics investigations: MiddleLate Pleistocene syn-tectonic travertine deposition at Serre di Rapolano (Northern Apennines, Italy) (literal)
- Abstract
- Middle-Late Pleistocene tectonic activity has
been inferred through studies on travertine deposits
exposed in a tract of the hinterland Northern Apennines. A
detailed study on the relationships between tectonics and
travertine deposition coupled with 230Th/234U age determination
of travertines at Cava Oliviera quarry, located
close to Serre di Rapolano village (southern Tuscany,
Northern Apennines), allowed us to recognise Pleistocene
faults, whose activity has been referred to 157-24 ka, at
least. Travertine deposition was tectonically controlled by
WSW-ENE striking, oblique and normal faults, associated
to a main fault (named as the Violante Fault). This structure
dissected a regional normal fault (known as the
Rapolano Fault) Early-Middle Pliocene in age, which
bounded the eastern side of the Pliocene Siena Basin, and
gave rise to space accommodation for clayey and sandy
marine sediments. Hydrothermal circulation (and related
travertine deposition) was favoured by the damaging
enhancement due to the fault-fault intersection. Tectonic
activityhasbeenalsodocumentedbydeformationrecorded
by travertines, which suggest a main tectonic event
between 64± 5 and 40± 5 ka. The tectonic activity
described for the study area agrees with the Quaternary
tectonic evolution documented in the surrounding areas
(e.g. Mt. Amiata and Mt. Vulsini), as well as the Tyrrhenian
margin of the Central Apennines, indicating that a
widespread tectonic activity affected the inner part of the
Apennines until the latest Quaternary. (literal)
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