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大兴安岭北部森林沼泽区1:5万水系沉积物测量方法研究
引用本文:马晓阳,崔玉军,李祥佑.大兴安岭北部森林沼泽区1:5万水系沉积物测量方法研究[J].物探与化探,2002,26(6):433-435,449.
作者姓名:马晓阳  崔玉军  李祥佑
作者单位:[1]中国地质大学,北京100083 [2]黑龙江地质调查总院,黑龙江哈尔滨150036
摘    要:通过对在大兴安岭北部森林沼泽—冻土景观区的1:5万水系沉积物测量方法技术的研究,发现以水系沉积物中较粗粒级的碎屑(-10~+60目)作为采样介质,可有效地排除有机质的干扰,强化异常;并提出在水系沉积物不甚发育的地区,以水系沉积物为主,辅以网格法土壤测量,则能更有效地提高找矿效果。

关 键 词:风化作用  元素迁移与富集  水系沉积物  土壤  粒度  有机质
收稿时间:2001-12-03

TECHNIQUES OF1:50000 STREAM SEDIMENT SURVEY IN FOREST-SWAMP AREA OF NORTHERN DA HINGGAN MOUNTAINS
Institution:1. China Universcity of Geosciences, Beijing 100083, China;
2. Heilongjiang Institute of Geological Survey, Harbin 150036, China
Abstract:Based on a study of the techniques for 1:50000 stream sediment survey in forest swamp frozen soil landscape area of northern Da Hinggan Mountains, the authors have discovered that the adoption of relatively coarse grained fragments (-10~+60 mesh) in stream sediments can effectively eliminate the interference of organic matter and strengthen the anomaly. It is also held that in areas where stream sediments are not well developed, the utilization of stream sediment survey with the help of grid soil survey can obviously raise the ore prospecting efficiency.
Keywords:weathering  migration and enrichment of elements  stream sediments  soil  grain size  organic matter
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