Metamorphic evolution of eclogite and associated garnet-mica schist in the high-pressure metamorphic Maksyutov complex, Ural, Russia

1999 ◽  
Vol 87 (4) ◽  
pp. 561-576 ◽  
Author(s):  
B. Schulte ◽  
P. Blümel
Keyword(s):  
High Pressure ◽  
Mica Schist ◽  
Metamorphic Evolution ◽  
Maksyutov Complex

scholarly journals Metamorphic Evolution and Tectonic Implications of Garnet-Bearing Mica Schist in Sumdo High Pressure Belt from Eastern Lhasa Block, Tibet

2015 ◽  
Vol 89 (s2) ◽  
pp. 3-4 ◽  
Author(s):  
Mei CHEN ◽  
Jingsui YANG ◽  
Cong ZHANG ◽  
Zuolin TIAN ◽  
Jie HUANG ◽  
...  
Keyword(s):  
High Pressure ◽  
Mica Schist ◽  
Metamorphic Evolution ◽  
Tectonic Implications

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.

A moderate exhumation rate for the high-pressure Maksyutov Complex, southern Urals, Russia

2000 ◽  
Vol 35 (3-4) ◽  
pp. 327-344 ◽  
Author(s):  
Ralf Hetzel ◽  
Rolf L. Romer
Keyword(s):  
High Pressure ◽  
Southern Urals ◽  
Exhumation Rate ◽  
Maksyutov Complex

Subduction- and exhumation-related fabrics in the Paleozoic high-pressure–low-temperature Maksyutov Complex, Antingan area, southern Urals, Russia

1998 ◽  
Vol 110 (7) ◽  
pp. 916-930 ◽  
Author(s):  
Ralf Hetzel ◽  
Helmut P. Echtler ◽  
Wolfgang Seifert ◽  
Bernd A. Schulte ◽  
Kirill S. Ivanov
Keyword(s):  
High Pressure ◽  
Low Temperature ◽  
Southern Urals ◽  
Maksyutov Complex

Metamorphic evolution of high-pressure and ultrahigh-temperature granulites from the Highland Complex, Sri Lanka

2006 ◽  
Vol 28 (1) ◽  
pp. 20-37 ◽  
Author(s):  
Yasuhito Osanai ◽  
Krishnan Sajeev ◽  
Masaaki Owada ◽  
K.V.Wilbert Kehelpannala ◽  
W.K.Bernard Prame ◽  
...  
Keyword(s):  
High Pressure ◽  
Sri Lanka ◽  
Metamorphic Evolution ◽  
Ultrahigh Temperature
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