大别山超高压硬玉石英岩中的水: 来自红外光谱的证据

樊孝玉; 吴秀玲; 孟大维; 刘卫平; 汪新星; 郑建平

Volume 32 Issue 2

Mar. 2007

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Article Navigation > Earth Science > 2007 > 32(2): 167-174

FAN Xiao-yu, WU Xiu-ling, MENG Da-wei, LIU Wei-ping, WANG Xin-xing, ZHENG Jian-ping, 2007. Water in UHP Jadeite-Quartzites of Dabie Mountains: Evidence from Micro-FTIR. Earth Science, 32(2): 167-174.

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FAN Xiao-yu, WU Xiu-ling, MENG Da-wei, LIU Wei-ping, WANG Xin-xing, ZHENG Jian-ping, 2007. Water in UHP Jadeite-Quartzites of Dabie Mountains: Evidence from Micro-FTIR. Earth Science, 32(2): 167-174.

FAN Xiao-yu, WU Xiu-ling, MENG Da-wei, LIU Wei-ping, WANG Xin-xing, ZHENG Jian-ping, 2007. Water in UHP Jadeite-Quartzites of Dabie Mountains: Evidence from Micro-FTIR. Earth Science, 32(2): 167-174.

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Water in UHP Jadeite-Quartzites of Dabie Mountains: Evidence from Micro-FTIR

1.
Faculty of Materials Science and Chemical Engineering, China University of Geosciences, Wuhan 430074, China
2.
Testing Center, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2006-10-30
Publish Date: 2007-03-25

Abstract

Abstract

The distribution characteristics of structural water in nominally anhydrous minerals (NAMs) from Dabie mountains can provide important microscopic information on some aspects of the related fluid activities, mineral deformation, dynamical process of blocks subduction and exhumation. The NAMs such as jadeites, garnets, rutiles and quarts in ultra-high pressure (UHP) jadeite-quartzites of Shuanghe and Bixiling areas from Dabie mountains were investigated by Fourier transform infrared spectroscopy (FTIR), the result of which indicates that NAMs contain hydrogen occurring as hydroxyl (OH^-) or molecule H₂O. It is found that the average structural water contents of the jadeites from the two areas are both close to 1 000×10^-6; the rutilezs' are both above 2 000×10^-6; the quarts' are both < 4×10^-6. The structural water contents of garnets from different grains in the same area aren't uniform, while the water contents of UHP jadeite-quartzites from the two areas both range from 900×10^-6 to 1 600×10^-6. The results reveal that the water in crust or protolith can be transported into the earth's depth through NAMs in the UHP metamorphic rocks during the formation of the HP-UHP metamorphic rocks.
- ultra-high pressure jadeite-quartzites,
- the structural water,
- NAMs,
- infrared spectroscopy,
- Dabie mountains

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References(56)

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Water in UHP Jadeite-Quartzites of Dabie Mountains: Evidence from Micro-FTIR

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