Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps

The Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence of Triassic to Jurassic rifting and Alpine orogen...

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Main Authors: L. Tavazzani, S. Peres, S. Sinigoi, G. Demarchi, G. Musumeci
Format: Article
Language:English
Published: Taylor & Francis Group 2017-11-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2017.1354787
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author L. Tavazzani
S. Peres
S. Sinigoi
G. Demarchi
G. Musumeci
author_facet L. Tavazzani
S. Peres
S. Sinigoi
G. Demarchi
G. Musumeci
author_sort L. Tavazzani
collection DOAJ
description The Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence of Triassic to Jurassic rifting and Alpine orogeny, the VMP and surrounding host rocks have been tilted more than 60° from their original Permian polarity. Thus at present day, the VMP offers the rare opportunity to study a roof-to-floor exposure of a granitic pluton, providing insights into pristine geometry of the magma chamber and its relations to the country rocks. This work presents a new drift and solid map of the VMP and its surrounding host rocks at 1:15.000 scale.
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spelling doaj.art-6d8a1bce34dc42749a865fce9205196d2022-12-22T00:52:57ZengTaylor & Francis GroupJournal of Maps1744-56472017-11-0113268469710.1080/17445647.2017.13547871354787Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern AlpsL. Tavazzani0S. Peres1S. Sinigoi2G. Demarchi3G. Musumeci4Southern Methodist UniversityUniversità di PisaUniversità di TriesteUniversità di TriesteUniversità di PisaThe Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence of Triassic to Jurassic rifting and Alpine orogeny, the VMP and surrounding host rocks have been tilted more than 60° from their original Permian polarity. Thus at present day, the VMP offers the rare opportunity to study a roof-to-floor exposure of a granitic pluton, providing insights into pristine geometry of the magma chamber and its relations to the country rocks. This work presents a new drift and solid map of the VMP and its surrounding host rocks at 1:15.000 scale.http://dx.doi.org/10.1080/17445647.2017.1354787Ivrea-Verbano ZoneSesia Magmatic Systemgranitic facieszoned plutonroof-to-floor exposure
spellingShingle L. Tavazzani
S. Peres
S. Sinigoi
G. Demarchi
G. Musumeci
Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps
Journal of Maps
Ivrea-Verbano Zone
Sesia Magmatic System
granitic facies
zoned pluton
roof-to-floor exposure
title Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps
title_full Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps
title_fullStr Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps
title_full_unstemmed Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps
title_short Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps
title_sort structure and petrography of the valle mosso pluton sesia magmatic system southern alps
topic Ivrea-Verbano Zone
Sesia Magmatic System
granitic facies
zoned pluton
roof-to-floor exposure
url http://dx.doi.org/10.1080/17445647.2017.1354787
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