ANISOTROPIC ETCHING OF CHARGED-PARTICLE TRACKS IN CRYSTALS.
被引:18
作者:
Dorung, G.W.
论文数: 0引用数: 0
h-index: 0
机构:
Department of Physics, University of Birmingham, Birmingham,B15 2TT, United KingdomDepartment of Physics, University of Birmingham, Birmingham,B15 2TT, United Kingdom
Dorung, G.W.
[1
]
Bull, R.K.
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h-index: 0
机构:
Department of Physics, University of Birmingham, Birmingham,B15 2TT, United KingdomDepartment of Physics, University of Birmingham, Birmingham,B15 2TT, United Kingdom
Bull, R.K.
[1
]
Durrani, S.A.
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h-index: 0
机构:
Department of Physics, University of Birmingham, Birmingham,B15 2TT, United KingdomDepartment of Physics, University of Birmingham, Birmingham,B15 2TT, United Kingdom
Durrani, S.A.
[1
]
Fremlin, J.H.
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h-index: 0
机构:
Department of Physics, University of Birmingham, Birmingham,B15 2TT, United KingdomDepartment of Physics, University of Birmingham, Birmingham,B15 2TT, United Kingdom
Fremlin, J.H.
[1
]
Khan, H.A.
论文数: 0引用数: 0
h-index: 0
机构:
Department of Physics, University of Birmingham, Birmingham,B15 2TT, United KingdomDepartment of Physics, University of Birmingham, Birmingham,B15 2TT, United Kingdom
Khan, H.A.
[1
]
机构:
[1] Department of Physics, University of Birmingham, Birmingham,B15 2TT, United Kingdom
来源:
Radiation Effects
|
1974年
/
23卷
/
02期
关键词:
Etching;
D O I:
10.1080/00337577408232056
中图分类号:
O48 [固体物理学];
学科分类号:
070205 ;
0805 ;
080502 ;
0809 ;
摘要:
It is well known that highly-energetic heavily charged particles arising both from the fissioning of heavy elements and from cosmic and solar radiations leave tracks which have been found in glasses and crystalline minerals recovered from lunar and meteoritic material. It has been shown that an appropriate analysis of these tracks can provide information about periods since solidification and the thermal and dynamic history of the specimen, as well as insight into the nature and temporal variation of the cosmic ray flux. An understanding of the track registration characteristics of crystals is clearly an important prerequisite to an appropriate interpretation of the natural tracks. This letter describes briefly some observations recently made on one particular aspect of this - the anisotropy in track distributions which seems to result from the inherently anisotropic structure of crystals. This effect seems so far to have received little attention.