Research output: Contribution to journal › Article › peer-review
High-Grade Metamorphism and Anatexis in the Teletskoe-Chulyshman Belt (Gorny Altai) : U-Pb Geochronology, P-T Estimates, and Thermal Tectonic Model. / Polyansky, O. P.; Kargopolov, S. A.; Babichev, A. et al.
In: Russian Geology and Geophysics, Vol. 60, No. 12, 12.2019, p. 1425-1443.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - High-Grade Metamorphism and Anatexis in the Teletskoe-Chulyshman Belt (Gorny Altai)
T2 - U-Pb Geochronology, P-T Estimates, and Thermal Tectonic Model
AU - Polyansky, O. P.
AU - Kargopolov, S. A.
AU - Babichev, A.
AU - Reverdatto, V. V.
PY - 2019/12
Y1 - 2019/12
N2 - A model of the formation of the Teletskoe-Chulyshman metamorphic belt (TCMB) in Gorny Altai has been elaborated. The estimated pressure (not exceeding 3-4 kbar) and temperature (about 740 ºС) indicate an increased regional crustal thermal gradient equal to 60-90 ºС/km during the formation of the metamorphic belt. The age of migmatites of the Chulyshman complex has been evaluated at 483.9 ± 5.7 Ma (Early Ordovician) by U/Pb (SHRIMP) zircon dating. The paleogeodynamic setting of the TCMB formation and the protolith nature are identified based on the geochemical and petrochemical parameters of the metamorphic rocks. Structural parameters and numerical modeling show that the Chulyshman migmatite-gneiss complex is an apical part of the thermal-dome structure formed under the thermal impact of a magmatic basic heat source in the base of the crust and displaced to the relevant depths via thrusts and crustal extrusion during the Early Ordovician accretion-collision event. Matching the metamorphism parameters and the numerical-modeling results for the crustal thermal regime, we determined the rate of the anatectic front displacement along the thrust to be at least 6 cm/yr.
AB - A model of the formation of the Teletskoe-Chulyshman metamorphic belt (TCMB) in Gorny Altai has been elaborated. The estimated pressure (not exceeding 3-4 kbar) and temperature (about 740 ºС) indicate an increased regional crustal thermal gradient equal to 60-90 ºС/km during the formation of the metamorphic belt. The age of migmatites of the Chulyshman complex has been evaluated at 483.9 ± 5.7 Ma (Early Ordovician) by U/Pb (SHRIMP) zircon dating. The paleogeodynamic setting of the TCMB formation and the protolith nature are identified based on the geochemical and petrochemical parameters of the metamorphic rocks. Structural parameters and numerical modeling show that the Chulyshman migmatite-gneiss complex is an apical part of the thermal-dome structure formed under the thermal impact of a magmatic basic heat source in the base of the crust and displaced to the relevant depths via thrusts and crustal extrusion during the Early Ordovician accretion-collision event. Matching the metamorphism parameters and the numerical-modeling results for the crustal thermal regime, we determined the rate of the anatectic front displacement along the thrust to be at least 6 cm/yr.
KW - P-T parameters
KW - thermal tectonic model
KW - U/Pb age
KW - high-temperature/low-pressure metamorphism
KW - Teletskoe-Chulyshman metamorphic belt
KW - Gorny Altai
KW - META-SEDIMENTARY ROCKS
KW - EVOLUTION
KW - CRUSTAL
KW - GEODYNAMICS
KW - GRANITE
KW - MANTLE
KW - REGION
KW - CONSTRAINTS
KW - PROVENANCE
KW - SAYAN
KW - Thermal tectonic model
KW - High-temperature/low-pressure metamorphism
UR - http://www.scopus.com/inward/record.url?scp=85089101795&partnerID=8YFLogxK
U2 - 10.15372/RGG2019108
DO - 10.15372/RGG2019108
M3 - Article
VL - 60
SP - 1425
EP - 1443
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 12
ER -
ID: 23288213