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矿井断层复杂程度系数的几何方法评价

Assessment on geometric method for complexity degree coefficient of mine fault

  • 摘要: 基于目前矿井断层复杂程度定量分析过程中,经常遇到一个断层复杂程度系数对应于多种地质客观实际,且其值偏小的问题。在评价前人采用的垂直落差面积比法和平错面积比法的基础上,采取断层倾斜间隔乘以断层延伸长度之和与统计单元面积之比来度量断层复杂程度。通过几何分析,提出了新的更为符合地质客观实际的几何模型,结果表明得出的断层复杂程度系数计算公式不具多解性,而且明了易懂,便于推广应用。

     

    Abstract: Based on the current quantitative analysis course of fault complexity degree in mine ,single fault complexity coefficient represents various geologic facts and its value was less than the fact. Based on the evaluation of sheer incline area ratio and strike-slip fault area ratio about former resea rch,measure fault complexity degree could take an inclined fault interval multiply by the sum of extension length and ratio of numerical statement area. By geometric analysis,the new geometric model was put forward which represented geologic facts in truth. The results indicated that new expression ed uced from the model had no multiplicity,and was transpicuous and convenient for popularization.

     

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