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- W2351285648 abstract "A sequence of middle-high-pressure metamorphic rocks occurs in the Heilongjiang Complex, whose representative lithology is blueschist and mica schist. Characteristic minerals of middle-high-pressure metamorphism, such as glaucophane, ferro-glaucophane and phengite (Si=3.37 to 3.463.30) are observed in the metamorphic rocks. The rock association, blueschist and mica schist, has suffered at least two stages of metamorphism. The P-T conditions are estimated to be 320 to 460 ℃ and 7.8×108 to 11×108 Pa, which correspond to early stage epidote-blueschist facies. The late stage is high-greenschist facies, which is characterized by the replacement of glaucophane and phengite by magnesium-rich (XMg=0.565 to 0.646) chlorite. The metamorphic conditions constrained by garnet mica schist are 536～598 ℃ and 6.8×108 to 9.5×108 Pa, consistent with medium temperature and middle-high pressure metamorphism." @default.
- W2351285648 created "2016-06-24" @default.
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- W2351285648 date "2013-01-01" @default.
- W2351285648 modified "2023-09-26" @default.
- W2351285648 title "Mineral Compositions and P-T Conditions of the Blueschist-Mica Schist in Heilongjiang Complex" @default.
- W2351285648 hasPublicationYear "2013" @default.
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