http://www.cnr.it/ontology/cnr/individuo/prodotto/ID274868
A new petro-structural map of the Monte Mucrone metagranitoids (SesiaLanzo Zone, Western Alps) (Articolo in rivista)
- Type
- Label
- A new petro-structural map of the Monte Mucrone metagranitoids (SesiaLanzo Zone, Western Alps) (Articolo in rivista) (literal)
- Anno
- 2013-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1080/17445647.2013.800004 (literal)
- Alternative label
Francesco Delleani [a], M. Iole Spalla [a b], Daniele Castelli [c], Guido Gosso [a b] (2013)
A new petro-structural map of the Monte Mucrone metagranitoids (SesiaLanzo Zone, Western Alps)
in Journal of maps; TAYLOR & FRANCIS LTD, London (Regno Unito)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Francesco Delleani [a], M. Iole Spalla [a b], Daniele Castelli [c], Guido Gosso [a b] (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://www.tandfonline.com/doi/pdf/10.1080/17445647.2013.800004 (literal)
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- [a]
Dipartimento di Scienza della Terra 'A. Desio', Universitàdi
Milano , Via Mangiagalli 34, 20133 , Milano , Italy
[b]
C.N.R.-I.D.P.A. , Sezione di Milano , Via Mangiagalli 34, 20133 ,
Milano , Italy
[c]
Dipartimento di Scienze della Terra , Universitàdi Torino , Via
Valperga Caluso 35, 10125 , Torino , Italy
Published online: 31 May 2013. (literal)
- Titolo
- A new petro-structural map of the Monte Mucrone metagranitoids (SesiaLanzo Zone, Western Alps) (literal)
- Abstract
- The Mt. Mucrone metagranitoid is an extensively investigated intrusive Permian body, located
in the Eclogitic Micaschists Complex of the Sesia-Lanzo Zone, within the high-pressure
metamorphic belt of the Western Alps formed during the Alpine plate convergence. The
structure of the northwestern sector of Mt. Mucrone, including both the metagranitoids and
country rocks, has been mapped, although an integrated structural and petrological analysis
is still lacking in its southwestern sector, a topic investigated in this contribution. During the
field structural analysis, six groups of ductile structures were recognized to have evolved as
follows: the D1 and D2 fabrics took place under eclogite-facies, D3 under blueschist-facies
and D4 to D6 under greenschist-facies conditions, respectively. Foliation trajectories
revealing the chronology of the superposed structures are represented in the analytical (drift
and solid) and interpretative (solid) maps, both at a 1:10,000 scale, and a panel of structural
cross-sections allows the 3D representation of the poly-deformed lithostratigraphy. The
related metamorphism indicates the changes within the subduction-collision tectonic frame. (literal)
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