中山大学学报(自然科学版)
中山大學學報(自然科學版)
중산대학학보(자연과학판)
ACTA SCIENTIARUM NATURALIUM UNIVERSITATIS SUNYATSENI
2014年
1期
148-154
,共7页
活动断裂%分形%网格覆盖法%历史地震活动%广东省
活動斷裂%分形%網格覆蓋法%歷史地震活動%廣東省
활동단렬%분형%망격복개법%역사지진활동%광동성
active faults%fractal%box-counting%historical seismic activities%Guangdong Province
以分形理论为基础,采用网格覆盖法,对广东省主要活动断裂进行分形研究。研究结果表明,广东省内主要活动断裂在分形标度区间12.5~100 km具有较好的统计自相似性,断裂分布的分形维数有效地描述了断裂的空间展布特征,全部断裂分形维数为1.5823,北东向断裂为1.4342,北西向断裂为1.1157和近东西向断裂1.0394,并且北东向断裂与北西向断裂的分布呈现一定的互补性。结合断裂分形维数等值线与历史地震活动,初步探讨了断裂分形维数与地震活动的耦合关系。
以分形理論為基礎,採用網格覆蓋法,對廣東省主要活動斷裂進行分形研究。研究結果錶明,廣東省內主要活動斷裂在分形標度區間12.5~100 km具有較好的統計自相似性,斷裂分佈的分形維數有效地描述瞭斷裂的空間展佈特徵,全部斷裂分形維數為1.5823,北東嚮斷裂為1.4342,北西嚮斷裂為1.1157和近東西嚮斷裂1.0394,併且北東嚮斷裂與北西嚮斷裂的分佈呈現一定的互補性。結閤斷裂分形維數等值線與歷史地震活動,初步探討瞭斷裂分形維數與地震活動的耦閤關繫。
이분형이론위기출,채용망격복개법,대광동성주요활동단렬진행분형연구。연구결과표명,광동성내주요활동단렬재분형표도구간12.5~100 km구유교호적통계자상사성,단렬분포적분형유수유효지묘술료단렬적공간전포특정,전부단렬분형유수위1.5823,북동향단렬위1.4342,북서향단렬위1.1157화근동서향단렬1.0394,병차북동향단렬여북서향단렬적분포정현일정적호보성。결합단렬분형유수등치선여역사지진활동,초보탐토료단렬분형유수여지진활동적우합관계。
Based on the fractal theory,the fractal geometry is applied to studying the active faults system in Guangdong Province.Results indicate that the spatial distribution of all faults in Guangdong Province is a distinct fractal set with self-similarity in the non-scale range of 12.5 -100 km,and the fractal dimen-sion,obtained by the box-counting method,interprets well the characteristics of the spatial distribution of faults.The fractal dimension of all faults in the study area is 1.582 3,that of the NE faults 1.434 2 and that of the NW faults 1.1 15 7 and EW faults 1.039 4.The densities of spatial distribution of the NE and the NW faults supplement to each other,indicating the inter-restraint properties of these two groups of faults.Eventually,correlating the isoline maps of fractal dimensions and historical earthquake distribu-tion,it is tried to find out the relationship between the fractal characteristics and seismic activities.