High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone

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High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone. / Likhanov, I. I.; Kozlov, P. S.; Ivanov, K. S. et al.

In: Doklady Earth Sciences, Vol. 483, No. 2, 01.12.2018, p. 1495-1498.

Research output: Contribution to journal › Article › peer-review

Author

Likhanov, I. I. ; Kozlov, P. S. ; Ivanov, K. S. et al. / High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone. In: Doklady Earth Sciences. 2018 ; Vol. 483, No. 2. pp. 1495-1498.

BibTeX

@article{90e7b51e8c0942aeb22f98d01233bb94,

title = "High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone",

abstract = "The occurrences of high-pressure tectonites localized in the tectonic suture zone of the Cis-Yenisei regional shear zone (CYRSZ) separated the cratonic and oceanic island-arc terranes were distinguished for the first time at the western margin of the Siberian Craton. Tectonites are characterized by high pressures (up to 15 kbar), which exceed significantly the background P-T parameters of regional metamorphism. The generation of tectonic overpressure is induced by rapid deformations along ductile shear zones, which is consistent with the numerical simulation results and thermodynamic calculations. These data confirm the important role of tectonic stress as an effective thermodynamic factor of metamorphic transformations in suture zones of the lithospheric crust.",

keywords = "GARNET, EVOLUTION, GEOBAROMETRY, EXHUMATION, ASSEMBLAGE, EVENTS, AGE",

author = "Likhanov, {I. I.} and Kozlov, {P. S.} and Ivanov, {K. S.} and Zinoviev, {S. V.}",

note = "Publisher Copyright: {\textcopyright} 2018, Pleiades Publishing, Ltd.",

year = "2018",

month = dec,

day = "1",

doi = "10.1134/S1028334X18120061",

language = "English",

volume = "483",

pages = "1495--1498",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "PLEIADES PUBLISHING INC",

number = "2",

}

RIS

TY - JOUR

T1 - High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone

AU - Likhanov, I. I.

AU - Kozlov, P. S.

AU - Ivanov, K. S.

AU - Zinoviev, S. V.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - The occurrences of high-pressure tectonites localized in the tectonic suture zone of the Cis-Yenisei regional shear zone (CYRSZ) separated the cratonic and oceanic island-arc terranes were distinguished for the first time at the western margin of the Siberian Craton. Tectonites are characterized by high pressures (up to 15 kbar), which exceed significantly the background P-T parameters of regional metamorphism. The generation of tectonic overpressure is induced by rapid deformations along ductile shear zones, which is consistent with the numerical simulation results and thermodynamic calculations. These data confirm the important role of tectonic stress as an effective thermodynamic factor of metamorphic transformations in suture zones of the lithospheric crust.

AB - The occurrences of high-pressure tectonites localized in the tectonic suture zone of the Cis-Yenisei regional shear zone (CYRSZ) separated the cratonic and oceanic island-arc terranes were distinguished for the first time at the western margin of the Siberian Craton. Tectonites are characterized by high pressures (up to 15 kbar), which exceed significantly the background P-T parameters of regional metamorphism. The generation of tectonic overpressure is induced by rapid deformations along ductile shear zones, which is consistent with the numerical simulation results and thermodynamic calculations. These data confirm the important role of tectonic stress as an effective thermodynamic factor of metamorphic transformations in suture zones of the lithospheric crust.

KW - GARNET

KW - EVOLUTION

KW - GEOBAROMETRY

KW - EXHUMATION

KW - ASSEMBLAGE

KW - EVENTS

KW - AGE

UR - http://www.scopus.com/inward/record.url?scp=85060315980&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18120061

DO - 10.1134/S1028334X18120061

M3 - Article

VL - 483

SP - 1495

EP - 1498

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 18632039