High crystalline quality of large single crystals of subglacial ice above Lake Vostok (Antarctica) revealed by hard X-ray diffraction

被引:27
作者
Montagnat, M
Duval, P
Bastie, P
Hamelin, B
Brissaud, O
de Angelis, MT
Petit, JR
Lipenkov, VY
机构
[1] CNRS, Lab Glaciol & Geophys Environm, F-38402 St Martin Dheres, France
[2] CNRS, Spectrometrie Phys Lab, F-38402 St Martin Dheres, France
[3] Inst Max Von Laue Paul Langevin, F-38042 Grenoble 9, France
[4] Arctic & Antarctic Res Inst, St Petersburg 199397, Russia
来源
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 2001年 / 333卷 / 08期
关键词
X-ray diffraction; ice monocrystals; Lake Vostok; Antarctica; abnormal grain growth;
D O I
10.1016/S1251-8050(01)01667-6
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
X-ray diffraction experiments were carried out on large ice crystals from accreted ice above Lake Vostok, a subglacial lake lying beneath the East Antarctic ice sheet. Results indicate a surprisingly very low lattice distortion. This crystalline quality does not seem to be affected by impurities. Abnormal grain growth should occur and could explain both the large grain size and the low lattice distortion. Accreted ice is therefore supposed to be non-plastically deforming. These results should be taken into account for further studies of the permeability of accreted ice to drilling fluid present in the borehole. (C) 2001 Academie des sciences / Editions scientifiques et medicales Elsevier SAS.
引用
收藏
页码:419 / 425
页数:7
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