CAJ | 학술논문

利用X射线荧光光谱仪(X-ray fluorescence spectrometer, 简写为XRF)对海南岛昌化江流域土壤样品和昌化江河口与邻近海域沉积物样品中的锆、钛元素进行了测试分析,并计算了样品中的锆、钛品位.研究结果表明,昌化江河口及其邻近海域沉积物中的锆、钛砂矿具有明显的异常富集;昌化江流域表层土壤中Zr和Ti呈含量变化大、高值相对集中分布的特点;主要母岩为大面积分布的花岗岩;炎热潮湿气候和河流的动力条件为母岩风化和含矿碎屑向海搬运的主要地质营力;沿岸显著的波浪和潮流作用及典型的砂砾质海岸为昌化江河口与邻近海域锆、钛砂矿的形成创造了有利条件.根据锆、钛品位计算结果圈定了南、北2个矿化远景区.
이용X사선형광광보의(X-ray fluorescence spectrometer, 간사위XRF)대해남도창화강류역토양양품화창화강하구여린근해역침적물양품중적고、태원소진행료측시분석,병계산료양품중적고、태품위.연구결과표명,창화강하구급기린근해역침적물중적고、태사광구유명현적이상부집;창화강류역표층토양중Zr화Ti정함량변화대、고치상대집중분포적특점;주요모암위대면적분포적화강암;염열조습기후화하류적동력조건위모암풍화화함광쇄설향해반운적주요지질영력;연안현저적파랑화조류작용급전형적사력질해안위창화강하구여린근해역고、태사광적형성창조료유리조건.근거고、태품위계산결과권정료남、북2개광화원경구.
This paper analyzes Zr and Ti of the topsoil samples obtained from the drainage of the Changhua River and the sediments collected from the Changhua River Estuary and its adjacent sea area using X-ray Fluorescence Spectrometer (XRF). The grade of Zr and Ti was calculated. The results show that Zr and Ti are enriched distinctly in the sediments of the Changhua River Estuary and its adjacent sea area, and that Zr and Ti in the topsoils of drainage of the river are characterized by large range of content and the relative concentration of high values. The main host rocks are the large-scale distributed granite, whose wheathering and debris transportation to the sea could have been mainly driven by the torridity and humid weather and river conditions. The significant coastal wave and tidal flow and the typical sandy and gravelly coast may have created favorable conditions for the formation of placer of Zr and Ti of the Changhua River estuary and its adjacent waters. The two mineralization prospect areas are confirmed. Further, two mineralization prospect areas are distinguished in terms of the grade of Zr and Ti. It is concluded that the geological conditions such as extensive distribution of granites, the climate of torridity and humidity, river hydraulic forcing, prominent tide and wave and typical gritty coast are in favor of the formation of Zr and Ti placers.