摘要
对多年来国内外测汞方法应用提出了新的看法，为测汞方法指出发展方向。认为汞气主要来源于构造断裂带，汞异常与各种类型矿体（汞矿体除外）并不一定有直接联系，矿体产生的汞异常只占无矿构造断裂带产生的汞异常的极少部分。认为测汞能够应用于地质工作中所有与构造断裂有关的领域。
The author puts forward a new view on the technology and application of the geochemical mercury survey which has been usedboth in China and abroad for years.This opinion points out the developing orientation of the mercury survey technology.It is held that mercury vapor comes mainly from structural faulted zones,that mercury anomalies are not necessarily in direct connection with various types of orebodies (except for mercury orebodies),and that mercury anomalies produced by orebodies are insignificant compared with mercury anomalies produced by barren structural faulted zones.It is also considered that mercury survey can be used in all geologic fieds related to structural faults.
出处
《物探与化探》
CAS
CSCD
1999年第1期21-27,共7页
Geophysical and Geochemical Exploration
关键词
地球化学
测汞
土壤吸附汞
构造断裂
破碎带
geochemistry
mercury survey
soil adsorbed mercury
structural fault
shatter zone
