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Modelling Synthesis in Laboratory of Coesite in the Earth's Crust and Its Formation Mechanism
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Shu-E LIU1, 2, Da-Peng XU1, Xiao-Mei LIU1, 2, Wen-Hui SU1, 4, Yan-Feng XUE1, Jing-Shu SUN1, 2
Chinese Journal of High Pressure Physics | 2006, 20(2) : 163 - 171
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Chinese Journal of High Pressure Physics | 2006, 20(2): 163-171
Modelling Synthesis in Laboratory of Coesite in the Earth's Crust and Its Formation Mechanism
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Shu-E LIU1, 2, Da-Peng XU1, Xiao-Mei LIU1, 2, Wen-Hui SU1, 4, Yan-Feng XUE1, Jing-Shu SUN1, 2
Affiliations
  • 1.Center for Rare-Earth Solid State Physics, Jilin University, Changchun 130023, China
  • 2.Center for the Condensed-Matter Science and Technology, Harbin Institute of Technology, and Key Laboratory of Condensed-Matter Science and Technology, Heilongjiang Provincial Universities, Harbin 150001, China
  • 3.International Center for Materials Physics, Academia Sinica, Shenyang 110015, China
  • 4.Center for Condensed Matter and Radiation Physics, China Center of Advanced Science and Technology (World Laboratory), Beijing 100080, China
Published: 2006-06-05
Outline
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The factors of collision and shear stress in the coesite formation has not been considered in the condition of high static pressure that was the base of the hypothesis of subduction-return of slab in the Earth. After considered these factors, a laboratory method of combining the high-energy mechanical ball milling (HEMBM) and high static pressure was suggested in this paper for modelling synthesis of coesite in the Earth's crust. A mechanical collision-induced intermediate phase of α-quartz has been discovered. Its condition of easily crystallizing into coesite induced by high static pressure is 3.0 GPa, 932 K, and < 1.0 min. The Raman peaks for the coesite synthesized by the present method have covered over the all information of those natural and synthesized coesite obtained before. This implicated that the coesite in the Earth's crust and subduction-return of slab maybe not come from as deep as common accepted value because of its lower pressure 3.0 GPa than that suggested by Jr. L. Coes. However, according to the fact discovered in this paper that the coesite could be synthesized under a condition of very short time (about 10 s) by the high static pressure after pre-treated of HEMBM, the intermediate phase of α-quartz could be transformed into coesite instantaneously by the interaction of an earthquake wave and/or stress. Therefore we suggest some other possible formation mechanisms for coesite in the Earth's crust and show that the coesite in the Earth's crust could record some information about the collision dynamics of plates and an earthquake wave.

quartz-coesite  /  high-energy mechanical ball milling  /  high static pressure  /  Raman spectroscopy  /  subduction-return of slab
刘曙娥, 许大鹏, 刘晓梅, 苏文辉, 薜燕峰, 孙敬姝. 地表柯石英的实验室模拟合成及其形成机制的研究. 高压物理学报, 2006 , 20 (2) : 163 -171 .
Shu-E LIU, Da-Peng XU, Xiao-Mei LIU, Wen-Hui SU, Yan-Feng XUE, Jing-Shu SUN. Modelling Synthesis in Laboratory of Coesite in the Earth's Crust and Its Formation Mechanism[J]. Chinese Journal of High Pressure Physics, 2006 , 20 (2) : 163 -171 .
Year 2006 volume 20 Issue 2
20
3
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Article Info
  • Receive Date:2005-01-18
  • Online Date:2026-11-01
  • Published:2006-06-05
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History
  • Received:2005-01-18
  • Revised:2005-04-25
Funding
Affiliations
    1.Center for Rare-Earth Solid State Physics, Jilin University, Changchun 130023, China
    2.Center for the Condensed-Matter Science and Technology, Harbin Institute of Technology, and Key Laboratory of Condensed-Matter Science and Technology, Heilongjiang Provincial Universities, Harbin 150001, China
    3.International Center for Materials Physics, Academia Sinica, Shenyang 110015, China
    4.Center for Condensed Matter and Radiation Physics, China Center of Advanced Science and Technology (World Laboratory), Beijing 100080, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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