黑龙江杂岩蓝片岩-云母片岩矿物成分及变质作用<i>P</i>-<i>T</i>条件

李蓉; 孙德有; 铃木和博; 郑常青

doi:10.3799/dqkx.2013.028

Volume 38 Issue 2

Mar. 2013

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Article Navigation > Earth Science > 2013 > 38(2): 277-288

LI Rong, SUN De-you, Suzuki Kazuhiro, ZHENG Chang-qing, 2013. Mineral Compositions and P-T Conditions of the Blueschist-Mica Schist in Heilongjiang Complex. Earth Science, 38(2): 277-288. doi: 10.3799/dqkx.2013.028

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LI Rong, SUN De-you, Suzuki Kazuhiro, ZHENG Chang-qing, 2013. Mineral Compositions and P-T Conditions of the Blueschist-Mica Schist in Heilongjiang Complex. Earth Science, 38(2): 277-288. doi: 10.3799/dqkx.2013.028

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Mineral Compositions and P-T Conditions of the Blueschist-Mica Schist in Heilongjiang Complex

doi: 10.3799/dqkx.2013.028

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
The Center for Chronological Research, Nagoya Uniwersity, Nagoya 464-8602, Japan

Received Date: 2012-04-15
Publish Date: 2013-03-01

Abstract

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 3.46 > 3.30) 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 (X_Mg=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.
- blueschist,
- mica schist,
- mineral compositions,
- Heilongjiang complex,
- petrology,
- geochemistry

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References(38)

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Mineral Compositions and P-T Conditions of the Blueschist-Mica Schist in Heilongjiang Complex

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