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A STUDY ON THE SAND OF FLAMING MOUNTAIN

A STUDY ON THE SAND OF FLAMING MOUNTAIN

Zhang Guilin
Chen Shaorong
S Ambe
K Maeda
K Suzuki
Y Sasa
E Yagi
H Yabuki
Z W Huang
F Ambe
Nuclear Science and TechniquesVol.3, No.2pp.69-72Published in print 01 May 1992
21800

A sand sample collected at the foot of Flaming Mountain was studied further. On the basis of the change in the relative intensity after heat treatment, one of the sextets observed in its Mössbauer spectrum at liquid nitrogen temperature was ascribed to goethite. This result provides a useful information on the geological history of the region where the mountain is located.

Mössbauer spectroscopySand of flaming mountain
REFERENCES
[1] Ambe F, Ambe S, Huang Z W et al. Hyp Int, 1988, 41: 751.
[2] Kündig W, Bömmel H, Constabaris G et al. Phys Rev, 1966, 142: 327.
[3] Forsyth J B, Hedley I G, Johnson C E. J Phys C, 1968, 1: 179.
[4] Brož D, Strakova J, Šubrt J et al. Hyp Int, 1990, 54: 479.
[5] Vandenberghe R E, De Grave E, Landuydt C et al. Hyp Int, 1990, 53: 175.
[6] Sun Zhoucheng, Private communication.