越南东北索陶-桑丹地区多金属成矿地球化学资料的统计评价

IF 0.4 Q4 ENVIRONMENTAL SCIENCES
Pham Nhu Sang, N. Phuong, Vu Thai Linh, B. V. Sang
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引用次数: 2

摘要

在越南东北部,Suoi Thau-Sang Than被认为是多金属矿床的高潜力地区。利用地球化学样品1720份进行了多金属成矿研究;通过统计分析和多元分析,确定了东北部分地区的地球化学异常,即索陶、桑丹、班克普等。地球化学数据的统计方法和聚类分析表明,Cu、Pb和Zn元素是较好的指标,且大部分符合对数正态分布或伽马分布。基于三阶阈值,Cu、Pb、Zn元素含量的地球化学异常反映了成矿带内铜成矿矿体的富集程度,并清晰地表明了三个不同带的富集程度。通过趋势面分析确定各指标元素与异常区之间的空间变化和关系,揭示了指标元素含量的相对变化,具有一定的规律性。拟合优度得到的Pb、Zn、Cu元素的趋势函数为三度趋势面模型。这些结果表明,该模型可用于研究索都-桑丹地区的地球化学异常和分析指示元素的浓度趋势。此外,统计分析表明,利用该地区底河沉积物进行多金属成矿研究具有显著的潜力。此外,地球化学数据还有助于评价探路者元素的地球化学异常和越南东北部索陶-桑丹地区的潜在矿物填图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Statistical evaluation of the geochemical data for prospecting polymetallic mineralization in the Suoi Thau – Sang Than region, Northeast Vietnam
In Northeast Vietnam, Suoi Thau-Sang Than is considered as a high potential area of polymetallic deposits. 1,720 geochemical samples were used to investigate polymetallic mineralization; thereby polymetallic ore occurrences in this study region were discovered and the statistical and multivariate analysis helps to define geochemical anomalies in some northeastern regions, namely Suoi Thau, Sang Than, and Ban Kep. The statistical method and cluster analysis of geochemical data indicate that the Cu, Pb, and Zn elements are good indicators, and most of them comply with the lognormal or gamma distribution. Based on the third-order threshold, the geochemical anomalies of the content of the Cu, Pb, and Zn elements reflect the concentration of copper forming ore bodies in the mineralized zone, and clearly show the concentration in three distinct zones. The trend surface analysis which was employed to determine spatial variations and relationships among these good indicator elements and anomalous areas revealed relative changes in the content of the indicator elements, and they can be considered as regular. Moreover, the goodness of fit obtained trend functions of Pb and Zn, and Cu elements is a third-degree trend surface model. These results indicate that the models can be useful in studying geochemical anomalies and analyzing the tendency of the concentration of indicator elements in the Suoi Thau-Sang Than region. Additionally, it is suggested that the statistical analysis shows a remarkable potential to use the bottom river sediments in the region to investigate polymetallic mineralization. Moreover, geochemical data can help to evaluate geochemical anomalies of the pathfinder elements and potential mineral mapping of the Suoi Thau-Sang Than region in Northeast Vietnam.
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