The metamorphic evolution of garnet-cordierite-sillimanite-gneisses of the Gruf-Complex, Eastern Pennine Alps

1983 ◽  
Vol 84 (2-3) ◽  
pp. 215-227 ◽  
Author(s):  
Kurt Bucher -Nurminen ◽  
Giles Droop
Keyword(s):  
Metamorphic Evolution ◽  
Gruf Complex

scholarly journals Reaction Textures and Metamorphic Evolution of Sapphirine-bearing Granulites from the Gruf Complex, Italian Central Alps

1984 ◽  
Vol 25 (3) ◽  
pp. 766-803 ◽  
Author(s):  
G. T. R. DROOP ◽  
K. BUCHER-NURMINEN
Keyword(s):  
Central Alps ◽  
Metamorphic Evolution ◽  
Gruf Complex

Structural and metamorphic evolution during tectonic mixing: is the Rocca Canavese Thrust Sheet (Italian Western Alps) a subduction-related mélange?

2018 ◽  
Vol 137 (2) ◽  
pp. 311-329 ◽  
Author(s):  
Manuel Roda ◽  
Francesca De Salvo ◽  
Michele Zucali ◽  
Maria Iole Spalla
Keyword(s):  
Western Alps ◽  
Metamorphic Evolution ◽  
Thrust Sheet

Les argiles triasiques du Maroc et leur évolution diagénétique et métamorphique. Triassic clays of Morocco and their diagenetic and metamorphic evolution

1987 ◽  
Vol 40 (3) ◽  
pp. 285-293 ◽  
Author(s):  
Saâd Benchekroun ◽  
Alain Piqué ◽  
Jacques Lucas ◽  
Yves Besnus ◽  
Dominique Robillard
Keyword(s):  
Metamorphic Evolution

Metamorphic evolution of metapelites in the high-pressure terrane of the Rhodope Zone, northern Greece

1993 ◽  
Vol 31 (2) ◽  
pp. 401-424 ◽  
Author(s):  
E. Mposkos ◽  
A. Liati
Keyword(s):  
High Pressure ◽  
Northern Greece ◽  
Metamorphic Evolution

EXHUMATION OF LOWER CRUSTAL UHT ROCKS INTO THE UPPER AMPHIBOLITE FACIES MIDDLE CRUST: THE GRUF COMPLEX, EUROPEAN CENTRAL ALPS

2016 ◽  
Author(s):  
Jeffrey Oalmann ◽  
◽  
Andreas Möller ◽  
Romain Bousquet
Keyword(s):  
Amphibolite Facies ◽  
Central Alps ◽  
Middle Crust ◽  
European Central ◽  
Gruf Complex ◽  
Lower Crustal

METAMORPHIC EVOLUTION AND METASOMATISM IN THE TSO MORARI UHP TERRANE, NW INDIA: CONSTRAINTS FROM GEOCHEMISTRY, FE ISOTOPES, AND THERMODYNAMIC MODELING

2018 ◽  
Author(s):  
Ruiguang PAN ◽  
◽  
Catherine A. Macris ◽  
Carrie A. Menold ◽  
Anat Shahar
Keyword(s):  
Thermodynamic Modeling ◽  
Metamorphic Evolution ◽  
Fe Isotopes ◽  
Tso Morari

STRUCTURAL AND METAMORPHIC EVOLUTION OF THE CONNECTICUT VALLEY-GASPÉ TROUGH – INSIGHTS FROM SOUTHERN QUEBEC AND NORTHERN VERMONT

2018 ◽  
Author(s):  
Morgann Gwenva Perrot ◽  
◽  
Alain Tremblay ◽  
Gilles Ruffet ◽  
Loic Labrousse ◽  
...  
Keyword(s):  
Metamorphic Evolution ◽  
Connecticut Valley

scholarly journals Metasediments Covering Ophiolites in the HP Internal Belt of the Western Alps: Review of Tectono-Stratigraphic Successions and Constraints for the Alpine Evolution

Minerals ◽  
2021 ◽  
Vol 11 (4) ◽  
pp. 411
Author(s):  
Paola Tartarotti ◽  
Silvana Martin ◽  
Andrea Festa ◽  
Gianni Balestro
Keyword(s):  
High Pressure ◽  
Western Alps ◽  
Metamorphic Evolution ◽  
Alpine Orogeny ◽  
Sedimentary Evolution ◽  
Hp Metamorphism ◽  
Tethys Ocean ◽  
Depositional Setting ◽  
Oceanic Rocks ◽  
Outer Band

Ophiolites of the Alpine belt derive from the closure of the Mesozoic Tethys Ocean that was interposed between the palaeo-Europe and palaeo-Adria continental plates. The Alpine orogeny has intensely reworked the oceanic rocks into metaophiolites with various metamorphic imprints. In the Western Alps, metaophiolites and continental-derived units are distributed within two paired bands: An inner band where Alpine subduction-related high-pressure (HP) metamorphism is preserved, and an outer band where blueschist to greenschist facies recrystallisation due to the decompression path prevails. The metaophiolites of the inner band are hugely important not just because they provide records of the prograde tectonic and metamorphic evolution of the Western Alps, but also because they retain the signature of the intra-oceanic tectono-sedimentary evolution. Lithostratigraphic and petrographic criteria applied to metasediments associated with HP metaophiolites reveal the occurrence of distinct tectono-stratigraphic successions including quartzites with marbles, chaotic rock units, and layered calc schists. These successions, although sliced, deformed, and superposed in complex ways during the orogenic stage, preserve remnants of their primary depositional setting constraining the pre-orogenic evolution of the Jurassic Tethys Ocean.

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