This study presents new field, structural and petrographic data (supported by geological map) on a portion of the southern Dora-Maira Massif (Western Alps), with implications for its tectono-stratigraphic and tectonometamorphic architecture. The southern Dora-Maira Massif is a tectonic nappe stack consisting of several continental crust units which underwent (ultra)-high pressure ((U)HP) metamorphism during the Alpine orogenesis. The study area is located in the Valmala Valley, immediately south of the well-known UHP Brossasco-Isasca Unit. Here, from lower to upper structural levels, are exposed a quartz-eclogitic unit (Rocca Solei Unit; RSU) and a blueschist unit (Dronero-Sampeyre Unit; DSU). At the contact between the RSU and DSU a shear zone has been recognized (here addressed as Valmala Shear Zone; VSZ). The VSZ lower portion is characterized by blocks of metabasite, serpentinite and calchschist, lenticular in shape and up to hundreds of meters in size, embedded in a matrix dominated by micaschist locally rich in carbonates. On the contrary, the upper portion of the VSZ contains blocks of micro-augen gneiss and minor impure marble, lenticular to tabular in shape and up to tens of meters wide, embedded in a matrix of micaschist. In the DSU, a metasedimentary Polymetamorphic Complex has been recognised on the basis of the occurrence of relict pre-Alpine porfiroblastic garnet, and distinguished from a Monometamorphic Complex mostly consisting of metavolcanic rocks. The structural setting of the DSU + VSZ is the result of two principal deformation stages (D1 and D2). The D1 is responsible for the development of a HP foliation (S1) marked by Gln + Grt ±Zo ±Ru in the metabasite and Ctd + Grt + white mica ±Gln ±Lws ±Ru in the micaschist. The D2 generates km-scale folds and an axial plane foliation (S2) marked by low pressure mineral assemblages (Act + Chl + Ab ±Czo ±Ttn in the metabasite and white mica + Chl ±Ab ±Czo ±Ilm in the metapelite). Preliminary petrologic data on the metapelites from the DSU constrain peak P-T conditions at ca. 470°C, 19 kbar, in the lawsonite-blueschist facies.

Geological-structural and metamorphic study of the Southern Dora-Maira Massif in Valmala (Varaita Valley, Western Alps)

NOSENZO, FRANCESCO;Gianni Balestro;Chiara Groppo;Andrea Festa
2019-01-01

Abstract

This study presents new field, structural and petrographic data (supported by geological map) on a portion of the southern Dora-Maira Massif (Western Alps), with implications for its tectono-stratigraphic and tectonometamorphic architecture. The southern Dora-Maira Massif is a tectonic nappe stack consisting of several continental crust units which underwent (ultra)-high pressure ((U)HP) metamorphism during the Alpine orogenesis. The study area is located in the Valmala Valley, immediately south of the well-known UHP Brossasco-Isasca Unit. Here, from lower to upper structural levels, are exposed a quartz-eclogitic unit (Rocca Solei Unit; RSU) and a blueschist unit (Dronero-Sampeyre Unit; DSU). At the contact between the RSU and DSU a shear zone has been recognized (here addressed as Valmala Shear Zone; VSZ). The VSZ lower portion is characterized by blocks of metabasite, serpentinite and calchschist, lenticular in shape and up to hundreds of meters in size, embedded in a matrix dominated by micaschist locally rich in carbonates. On the contrary, the upper portion of the VSZ contains blocks of micro-augen gneiss and minor impure marble, lenticular to tabular in shape and up to tens of meters wide, embedded in a matrix of micaschist. In the DSU, a metasedimentary Polymetamorphic Complex has been recognised on the basis of the occurrence of relict pre-Alpine porfiroblastic garnet, and distinguished from a Monometamorphic Complex mostly consisting of metavolcanic rocks. The structural setting of the DSU + VSZ is the result of two principal deformation stages (D1 and D2). The D1 is responsible for the development of a HP foliation (S1) marked by Gln + Grt ±Zo ±Ru in the metabasite and Ctd + Grt + white mica ±Gln ±Lws ±Ru in the micaschist. The D2 generates km-scale folds and an axial plane foliation (S2) marked by low pressure mineral assemblages (Act + Chl + Ab ±Czo ±Ttn in the metabasite and white mica + Chl ±Ab ±Czo ±Ilm in the metapelite). Preliminary petrologic data on the metapelites from the DSU constrain peak P-T conditions at ca. 470°C, 19 kbar, in the lawsonite-blueschist facies.
2019
14th Emile Argand Conference on Alpine Geological Studies
Sion (CH)
04-06 Settembre 2019
Abstract Volume
Universitè de Lausanne
63
63
Francesco Nosenzo, Gianni Balestro, Chiara Groppo, Andrea Festa
File in questo prodotto:
File Dimensione Formato  
Nosenzo et al AW2019.pdf

Accesso aperto

Tipo di file: PDF EDITORIALE
Dimensione 106.04 kB
Formato Adobe PDF
106.04 kB Adobe PDF Visualizza/Apri

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2318/1712151
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus ND
  • ???jsp.display-item.citation.isi??? ND
social impact