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作 者:杨少平[1] 焦保权[2] 孙忠军[1] 张学君 徐仁廷[1] 陆学普[2] 潘文胜 卜祥宗
机构地区:[1]中国地质科学院地球物理地球化学勘查研究所,河北廊坊065000 [2]吉林省第五地质调查所,吉林九台130500 [3]黑龙江省地球物理勘察院,黑龙江哈尔滨150036
出 处:《物探与化探》2008年第5期480-487,共8页Geophysical and Geochemical Exploration
基 金:国土资源调查项目(200320130002)资助
摘 要:在森林沼泽景观区中低山亚景观条件下,通过4个研究区的试点工作认为:①以找寻小型以上规模矿床为目的的区域化探异常查证工作方法,以水系沉积物加密测量为佳,采样粒级-10^+60目,采样密度3~4点/km2。②采用B层残坡积土壤测量可以达到同样的目的;采样粒级-20目,采样密度4点/km2左右;采样布局为沿山脚和山脊的不规则测网。③在倒石堆发育区,可以采用采样密度6~7点/km2渗湿土测量方法进行异常追踪。④泥炭测量难以获得比较全面和客观的测区找矿前景信息,在区域化探异常追踪阶段最好不要选用。The follow-up methods for regional geochemical anomalies were studied in four areas with the forest-swamp middle-low mountain landscape. Some conclusions were summarized: (1) Stream sediment survey of -10 - + 60 mesh with sampling density of 3 - 4 samples/km^2 is a good method in search for small-large sized deposits; (2) pedogeochemical method collecting layer-B residual and slope materials of - 20 mesh is also a good method, which uses an irregular network with sampling density of about 4 samples/km^2 along piedmont and ridge; (3) soaked soil survey with 6 -7 samples/km^2 for follow-up in talus areas can be effectively used; (4) peat survey method should not be applied because it only provides poor information of mineralization.
分 类 号:P632[天文地球—地质矿产勘探]
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