RESEARCH |
The Sheared Mechanism of Spiral and Vortex Dislocation on Beryl Crystal |
Qi Li-jian (1) C.G. Zeng (2) Sun Da-lian (3) 1. Gemmological Institute, China University of Geosiences , Wuhan, 430074 , China; Abstract: Natural Beryl from Sichuan,China formed in under pneumatogenic hydrothermal condition has a characteristic low iron high alkali chemical composition; w ( K 2O £« Na 2O) ©ƒ 1.40%, w( FeO T) ©‚ 0.25%. The amount of w ( H 2O)varies between 2.70% and 3.30%. Other impurities amounting to less than 0.1%. Most of these beryl crystals grow in hexagonal thick slab along the c £û 0001 £ý with occasionally short hexagonal prism. Under normal growth condition, certain crystal faces such as the hexagonal prism faces or hexagonal bipyramid faces may be missing and the crystal adopt a unique lateral growth direction. Beryl crystal is usually made up of pinacoid c £û 0001 £ý£¬ hexagonal bipyramid p £û 10 Surface microtopography £¬ growth defects and growth mechanism of natural beryl are studied £¬ the testing methods of atomic force microscope £¨ AFM £©£¬ differential interference microscope £¨ DIM £© ¡¢ scanning electron microscope £¨ SEM £© and STEM are employed in the research. The results show £¨ Fig1-2 £© that there is well developed . hexagonal spiral growth dislocation on the largest face, pinacoid c{0001}. Partly adopting the sinistral spiral dislocation £¬ while the majority adopting the enclosed spiral dislocation, this demonstrates the symmetrical characteristic of a hexagonal crystal system. Within the spiral dislocation, the steps have about equal distance in spacing (0.4 ¡« 0.8 ¦Ì m) and height £¨ 2.5 ¡« 5nm £© ; Sinistral spiral dislocation has more perfect growth in the smaller m{10 of the inner boundary on the steps of the inner rings may appear zigzag and partially broken. Thickness of the spiral steps increase as it nears the vacant core reaching between 42 ¡« 50nm while decreasing dramatically outward. Due to the existence of other similar vortex dislocation, the growth rate of the s{11
The growth process of this type of beryl crystal belongs to an unbalanced and very complex process of phase change. This growth process is governed by a combination of various conditions in thermodynamics and dynamics. It is the result of physics, chemistry and geochemistry in combination. The growth mechanism of
crystals under different growing dynamics can be demonstrated through their microscale growth defects found on them. This is especially true to the spiral and vortex dislocations that are very sensitive to the changes in growing conditions. Besides showing the essential combination of physical, chemical and geochemical conditions, they also demonstrate the importance of the existence and movement of certain element in the metallogenic dynamics of the Earth. Key words: beryl crystal £» atomic force microscopy £» microscale vortex dislocation £» crystalline phase vortex nucleation |