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Table 1 Structural units of the South Cottian Alps (see map Fig. 3)

From: The Maira-Sampeyre and Val Grana Allochthons (south Western Alps): review and new data on the tectonometamorphic evolution of the Briançonnais distal margin

Acro-nyms

Name of tectonic units

Paleogeographic domain

Main lithologies

Metamorphic facies

QN

Queyras nappe

Piemonte-Liguria

Ocean

Radiolarites, marbles and calcschists with ophiolite bodies

Blueschist

MV

Monviso ophiolite complex

Mainly ophiolites with minor

metasediments

Eclogite

VG

Val Grana unit

“Prepiemonte” – type facies of the Briançonnais s.l. distal margin

Mesozoic metasediments

(Ladinian-Pliensbachian)

Blueschist

VM-S

Val Maira – Sampeyre unit

Permian-Mesozoic metasediments

(Upper Permian-Ladinian)

Blueschist

(cf. GS further N)

(cf. Giulian-Sea Bianca unit)

CLSZ

Cima Lubin shear zone

Shear zones representing tectonic mélanges of oceanic and margin units

Mesozoic metasediments (dolostones, calcschists) and minor ophiolite bodies

Blueschist

SDSZ

San Damiano shear zone

Blueschist

VPSZ

Valmala-Piasco shear zone

HT- blueschist

Drn2

Upper Dronero unit

Dora-Maira crystalline Massif representing part of the former basement of the Briançonnais s.l. distal margin

Polycyclic schists and monocyclic metased. and granites (Permian)

Quartz eclogite

Drn1

Lower Dronero unit

Polycyclic basement

Blueschist

R

Ricordone unit

Polycyclic basement

Quartz eclogite

RS

Rocca Solei unit

Polycyclic basement

Quartz eclogite

BI

Brossasco-Isasca unit

Polycyclic basement

Coesite eclogite

SP

Sanfront-Pinerolo unit

Monocyclic metasediments (Carboniferous- Triassic) + Permian

felsic intrusives

Garnet blueschist to eclogite

AL

Units of the Acceglio- Longet band (Acceglio anticline, Rocca Corna and Pelvo d’Elva units) and their southern equivalents

Acceglio-type facies domains of the Briançonnais s.l. distal margin (Acceglio, "Ecailles intermédiaires" or Ultrabriançonnais

auct.)

Monocyclic metasediments (Up. Carbon.-Up. Cretac.-Paleoc., with Middle Triassic—Liassic gap) + Permian felsites

Polycyclic schists (scarce)

HT- blueschist

CBR

Classical Briançonnais nappes or Briançonnais s. str. (various nappes, see Fig. 6)

Briançonnais proximal margin (= Briançonnais s.str. domain)

Cf. Acceglio units but with thick Middle ± Upper Triassic dolostones

 ± Lower Liassic (rare) + Eocene

“Flysch noir”

Greenschist to LT- blueschist

SBR

Subbriançonnais units

Valaisan and Subbriançonnais rift

domains

Up. Triassic (evaporites) – Eocene sediments

Non- metamorphic