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...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Taylor & Francis Group
2017-11-01
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| Series: | Journal of Maps |
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1080/17445647.2017.1354787 |