山东国土资源
山東國土資源
산동국토자원
LAND AND RESOURCES IN SHANGDONG PROVINCE
2012年
5期
17-20
,共4页
秦润君%吴虹%许浩%李敏%杨贤
秦潤君%吳虹%許浩%李敏%楊賢
진윤군%오홍%허호%리민%양현
断裂活动性%分形%模糊评判%多光谱遥感数据%闽南地区
斷裂活動性%分形%模糊評判%多光譜遙感數據%閩南地區
단렬활동성%분형%모호평판%다광보요감수거%민남지구
Activity of faults%fractal%fuzzy evalution%multi- spectral remoting sensing datas%Minnan area
以闽南地区为研究区域,以ETM+遥感影像数据为基础,通过广泛收集、分析研究区地质背景资料,分析区域内断层活动情况,进而提取研究区线性构造信息,结合地震地质资料对闽南地区主要断裂的分布情况及活动性做系统的分析研究。同时对闽南地区的新构造活动及构造应力场,线性构造和水系的分形分维,地震活动及其危险性和地热异常等主要影响因子做初步探讨。在确定影响断裂活动性的主要因素后,对研究区进行初步分区和定量化评价。最终判定研究区可圈定为:相对较不活动区、相对较活动区、相对活动区3个活动性级别。其中相对活动区面积占整个研究区3/5以上;相对较不活动区面积较小,造成相对活动的关键性因素是地震、活动断裂。
以閩南地區為研究區域,以ETM+遙感影像數據為基礎,通過廣汎收集、分析研究區地質揹景資料,分析區域內斷層活動情況,進而提取研究區線性構造信息,結閤地震地質資料對閩南地區主要斷裂的分佈情況及活動性做繫統的分析研究。同時對閩南地區的新構造活動及構造應力場,線性構造和水繫的分形分維,地震活動及其危險性和地熱異常等主要影響因子做初步探討。在確定影響斷裂活動性的主要因素後,對研究區進行初步分區和定量化評價。最終判定研究區可圈定為:相對較不活動區、相對較活動區、相對活動區3箇活動性級彆。其中相對活動區麵積佔整箇研究區3/5以上;相對較不活動區麵積較小,造成相對活動的關鍵性因素是地震、活動斷裂。
이민남지구위연구구역,이ETM+요감영상수거위기출,통과엄범수집、분석연구구지질배경자료,분석구역내단층활동정황,진이제취연구구선성구조신식,결합지진지질자료대민남지구주요단렬적분포정황급활동성주계통적분석연구。동시대민남지구적신구조활동급구조응력장,선성구조화수계적분형분유,지진활동급기위험성화지열이상등주요영향인자주초보탐토。재학정영향단렬활동성적주요인소후,대연구구진행초보분구화정양화평개。최종판정연구구가권정위:상대교불활동구、상대교활동구、상대활동구3개활동성급별。기중상대활동구면적점정개연구구3/5이상;상대교불활동구면적교소,조성상대활동적관건성인소시지진、활동단렬。
Taking Minnan area as a research area, based on ETM + remote sensing image datas, through collecting and analyzing geological background information, analyzing the activities of the faults, extrac- ting linear structure information, and combining with earthquake geological datas, distribution and activi- ties of main fractures in Minnan region have been analyzed and studied. Genozoic and recent techonic activ- ities, the crustal surface, fractal dimension of linear structures and river system, seismic activities, risks and geothermal abnormity have been studied primarily. Based on active analysis and fuzzy comprehensive evaluation, the active grade of each subzone in Minnan area has been determined. The research area can be finally circled into the relative not activity region, comparative activity region and the activity region. The relative activity region of area is more than three of five of the whole research area. The relative not activi- ty region is smaller. The key factors which caused realive activity are earthquake and active faults.