华南地质与矿产
華南地質與礦產
화남지질여광산
GEOLOGY AND MINERAL RESOURCES OF SOUTH CHINA
2014年
2期
124-130
,共7页
土壤地球化学测量%成矿元素%禾尚田钨多金属矿床
土壤地毬化學測量%成礦元素%禾尚田鎢多金屬礦床
토양지구화학측량%성광원소%화상전오다금속광상
soil geochemical survey%ore-forming elements%Heshangtian tungsten polymetallic deposit
本文通过分析禾尚田矿区1∶1万土壤测量成果,结合区域成矿地质条件和矿区矿床地质特征,对禾尚田钨锡多金属矿区成矿元素地球化学特征进行分析研究。结果表明:(1)各成矿元素具高背景、高浓集的特征,含量与地层具相关性,空间上具温度梯度分带;(2)成矿元素异常具分异与叠加特征,矿区受构造和地层双重控制,为多期次成矿;(3)成矿元素异常具找矿指示意义,据此可在区域与深部获找矿突破。
本文通過分析禾尚田礦區1∶1萬土壤測量成果,結閤區域成礦地質條件和礦區礦床地質特徵,對禾尚田鎢錫多金屬礦區成礦元素地毬化學特徵進行分析研究。結果錶明:(1)各成礦元素具高揹景、高濃集的特徵,含量與地層具相關性,空間上具溫度梯度分帶;(2)成礦元素異常具分異與疊加特徵,礦區受構造和地層雙重控製,為多期次成礦;(3)成礦元素異常具找礦指示意義,據此可在區域與深部穫找礦突破。
본문통과분석화상전광구1∶1만토양측량성과,결합구역성광지질조건화광구광상지질특정,대화상전오석다금속광구성광원소지구화학특정진행분석연구。결과표명:(1)각성광원소구고배경、고농집적특정,함량여지층구상관성,공간상구온도제도분대;(2)성광원소이상구분이여첩가특정,광구수구조화지층쌍중공제,위다기차성광;(3)성광원소이상구조광지시의의,거차가재구역여심부획조광돌파。
Based on the data of the 1:10,000 soil survey results, combines with the regional metallogenic geologi-cal conditions and geological features analysis, the metallogenic element geochemical characteristics of Heshang-tian deposit are studied in this paper. The results showed that: (1) characteristics of the ore-forming elements are with high background, high concentration, and correlated with the typical stratum, and in space with temperature gradient zone;(2) metallogenic element anomalies with abnormal differentiation and overlay feature, ore bodies are controlled by structural and stratigraphy, usually with multi-stage mineralization;(3) ore-forming element anoma-lies as prospecting significance can obtain breakthrough in the regional exploration.