Practical visualization of rock structure

被引:6
|
作者
Pusch, R [1 ]
机构
[1] Geodev AB, S-22370 Lund, Sweden
关键词
discontinuities; fracture zones; modeling; numerical codes; rock; structure;
D O I
10.1016/S0013-7952(97)00054-9
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The conventionally applied method for visualizing the structure of a rock mass is limited to plotting the orientation of individual discontinuities by using the Schmidt stereographic net. Their spacing is not illustrated and other structural features, such as undulation and twisting, cannot be interpreted from such stereographic views. A new mode of visual presentation of rock structural features of one or several different types in rock volumes of any size that makes all this possible is proposed in the present report. The primary purpose is to quantify, for all elements of a rock mass where the structure has been evaluated by borehole investigations or mapping in the course of underground excavation, the orientation and average spacing of defined discontinuities like hydraulically and mechanically active fractures. These local structural patterns, which are plotted on three of the six faces of cubical boxes with defined edge length and with one edge oriented N-S can be combined by applying the mathematical tool for connecting faces with which certain visualization codes like Alias Sketch are equipped. This combines different local rock structures to form regional patterns that can reveal undulation and twisting and important variations in spacing of major discrete discontinuities. Visualization can be given in true perspective or orthographic form and larger discontinuities that have been identified in the field, such as fracture zones. can be introduced in the model for correlation with smaller Features. Furthermore, the stress situation at all sites where rock stress measurements have been made can be visualized in the model in the form of principal planes. The proposed models can be visualized from any "camera angle" and also shown in Quick Time VR form. i.e. as being slowly rotated around any predetermined axis. This facilitates definition and selection of the rock structure, local or regional, for numerical calculations. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:231 / 236
页数:6
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