物探化探计算技术
物探化探計算技術
물탐화탐계산기술
COMPUTING TECHNIQUES FOR GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2014年
4期
487-491
,共5页
赵禹%赵玉岩%郝立波%陆继龙
趙禹%趙玉巖%郝立波%陸繼龍
조우%조옥암%학립파%륙계룡
背景上限%快速聚类%造岩元素%复杂岩性区
揹景上限%快速聚類%造巖元素%複雜巖性區
배경상한%쾌속취류%조암원소%복잡암성구
upper limit of geochemical background%K-Means cluster%rock-forming elements%complex lithology distract
区域化探原生背景与异常形成于相互独立的地质过程。在岩性复杂区,不同地质单元内背景与异常的成因可能完全不同,划定统一的背景上限显然是不科学的,合理的解决方案是分区确定化探背景上限。这里提出一种采用主要造岩元素为指标,采用快速聚类分析方法划分地质单元并分别计算背景上限的简便方法。以1:200000郴县幅化探数据为例进行试验,结果表明,该方法能有效地去除不同地质体类型背景对异常的影响,不仅能突出矿区异常,也能削弱高背景区非矿致异常,缩小靶区面积,识别微弱异常。
區域化探原生揹景與異常形成于相互獨立的地質過程。在巖性複雜區,不同地質單元內揹景與異常的成因可能完全不同,劃定統一的揹景上限顯然是不科學的,閤理的解決方案是分區確定化探揹景上限。這裏提齣一種採用主要造巖元素為指標,採用快速聚類分析方法劃分地質單元併分彆計算揹景上限的簡便方法。以1:200000郴縣幅化探數據為例進行試驗,結果錶明,該方法能有效地去除不同地質體類型揹景對異常的影響,不僅能突齣礦區異常,也能削弱高揹景區非礦緻異常,縮小靶區麵積,識彆微弱異常。
구역화탐원생배경여이상형성우상호독립적지질과정。재암성복잡구,불동지질단원내배경여이상적성인가능완전불동,화정통일적배경상한현연시불과학적,합리적해결방안시분구학정화탐배경상한。저리제출일충채용주요조암원소위지표,채용쾌속취류분석방법화분지질단원병분별계산배경상한적간편방법。이1:200000침현폭화탐수거위례진행시험,결과표명,해방법능유효지거제불동지질체류형배경대이상적영향,불부능돌출광구이상,야능삭약고배경구비광치이상,축소파구면적,식별미약이상。
Primary background and anomaly of regional geochemical exploration formed in independent geological processes. The causes of background and anomaly of different geological unit in complex lithology distract are completely different,so it is unreasonable to delineate the same upper limit of geochemical background.Reasonable solution is to determine the upper limit of geochemical background by subregion.A simple method of subregion determine of upper limit of geochemical background u-sing K-Means cluster analysis,which uses main rock-forming elements as indicator,was presented.A test was progressed using geochemical data of 1:200 000 Chenxian geological map,the results show that this method can effectively remove impact of different geological unit anomalies,and it can not only highlight the mine anomalies but also weaken the non-mining anoma-lies in high background areas,narrow target area and identify weak anomalies.