In Situ High-Pressure Synchrotron X-Ray Diffraction Study of Clinozoisite

	In Situ High-Pressure Synchrotron X-Ray Diffraction Study of Clinozoisite
	Fan, DW; Ma, MN; Yang, JJ; Wei, SY; Chen, ZQ; Xie, HS
	2011
发表期刊	CHINESE PHYSICS LETTERS
卷号	28 期号:12 页码:126103-1-126103-1-4
摘要	We investigate the elastic behavior of a natural clinozoisite under about 20.4GPa at 300K using in situ angle-dispersive x-ray diffraction and a diamond anvil cell at the National Synchrotron Light Source, Brookhaven National Laboratory. Over this pressure range, no phase change or disproportionation has been observed. The isothermal equation of state is determined. The values of.. 0 and.. 0 refined by the Murnaghan equation of state are V(0) = 460.0 +/- 0.2 angstrom(3), K(0) = 138 +/- 3 GPa. Consequently, it can be concluded that the compressibility of clinozoisite under high pressures is accurately constrained.
学科领域	地球深部物质与流体作用地球化学
收录类别	SCI
语种	英语
文献类型	期刊论文
条目标识符	http://ir.gyig.ac.cn/handle/352002/4891
专题	地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
推荐引用方式 GB/T 7714	Fan, DW,Ma, MN,Yang, JJ,et al. In Situ High-Pressure Synchrotron X-Ray Diffraction Study of Clinozoisite[J]. CHINESE PHYSICS LETTERS,2011,28(12):126103-1-126103-1-4.
APA	Fan, DW,Ma, MN,Yang, JJ,Wei, SY,Chen, ZQ,&Xie, HS.(2011).In Situ High-Pressure Synchrotron X-Ray Diffraction Study of Clinozoisite.CHINESE PHYSICS LETTERS,28(12),126103-1-126103-1-4.
MLA	Fan, DW,et al."In Situ High-Pressure Synchrotron X-Ray Diffraction Study of Clinozoisite".CHINESE PHYSICS LETTERS 28.12(2011):126103-1-126103-1-4.

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