Research output: Contribution to journal › Article › peer-review
Two episodes of metamorphism in the rocks of the eastern Kitoi block (Sharyzhalgai uplift of the Siberian platform) according to the Garnet amphibolite data. / Sukhorukov, V. P.; Savel'eva, V. B.
In: Geodynamics and Tectonophysics, Vol. 11, No. 1, 01.01.2020, p. 107-121.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Two episodes of metamorphism in the rocks of the eastern Kitoi block (Sharyzhalgai uplift of the Siberian platform) according to the Garnet amphibolite data
AU - Sukhorukov, V. P.
AU - Savel'eva, V. B.
N1 - Сухоруков В.П., Савельева В.Б. Две стадии метаморфизма в породах восточной части Китойского блока (Шарыжалгайский выступ Сибирской платформы) по данным изучения гранатовых амфиболитов // Геодинамика и тектонофизика. - 2020. - Т. 11. - № 1. - С. 107-121
PY - 2020/1/1
Y1 - 2020/1/1
N2 - The Archean metamorphism in the southwestern Siberian craton was confirmed by the studies of the Kitoy and Irkutsk blocks. However, the parameters of the metamorphism process are still poorly investigated. The article presents the first results of studying the metamorphism conditions of garnet amphibolites sampled from the Kitoy sillimanite deposit. The reaction relationships of the studied minerals give grounds to distinguish two episodes of the regional metamorphism. At the end of the first episode, (Т=710-770 °С and Р=8.3-8.8 kb), the pressure reduced to 1.3-2.5 kbar at T=700 °C at the retrograde stage, and amphibole-plagioclase rims formed around garnet grains. During the second episode of metamorphism, the temperature reached 890 °С (granulite facies), and Cpx+Opx paragenesis replaced hornblende. The second episode of metamorphism is not evident in all the samples (considering the same bulk rocks composition of the rocks), which suggests its local character.
AB - The Archean metamorphism in the southwestern Siberian craton was confirmed by the studies of the Kitoy and Irkutsk blocks. However, the parameters of the metamorphism process are still poorly investigated. The article presents the first results of studying the metamorphism conditions of garnet amphibolites sampled from the Kitoy sillimanite deposit. The reaction relationships of the studied minerals give grounds to distinguish two episodes of the regional metamorphism. At the end of the first episode, (Т=710-770 °С and Р=8.3-8.8 kb), the pressure reduced to 1.3-2.5 kbar at T=700 °C at the retrograde stage, and amphibole-plagioclase rims formed around garnet grains. During the second episode of metamorphism, the temperature reached 890 °С (granulite facies), and Cpx+Opx paragenesis replaced hornblende. The second episode of metamorphism is not evident in all the samples (considering the same bulk rocks composition of the rocks), which suggests its local character.
KW - Amphibolite
KW - Archean
KW - Granulite metamorphism
KW - Kitoy block
KW - P-T path of metamorphism
KW - PT-parameters
KW - Siberian craton
KW - Siberian craton
KW - Kitoy block
KW - Archean
KW - granulite metamorphism
KW - amphibolite
KW - PT-parameters
KW - P-T path of metamorphism
KW - SILLIMANITE SCHIST DEPOSIT
KW - IRKUT BLOCK
KW - RICH GRANULITES
KW - CRATON
KW - TEMPERATURE
KW - AGE
KW - EVOLUTION
KW - COMPLEX
KW - CALIBRATION
KW - THERMOBAROMETRY
UR - http://www.scopus.com/inward/record.url?scp=85086125656&partnerID=8YFLogxK
UR - https://www.elibrary.ru/item.asp?id=42656259
U2 - 10.5800/GT-2020-11-1-0466
DO - 10.5800/GT-2020-11-1-0466
M3 - Article
AN - SCOPUS:85086125656
VL - 11
SP - 107
EP - 121
JO - Geodynamics and Tectonophysics
JF - Geodynamics and Tectonophysics
SN - 2078-502X
IS - 1
ER -
ID: 24517850