Extraction of deep mineralization information from weak and low tectono-geochemical anomalies: A case study of the Maoping germanium-rich lead–zinc deposit in northeastern Yunnan Province, China

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Yixuan Yang, Gaoming Zhou, Runsheng Han, Hongsheng Gong, Jianbiao Wu, Yan Zhang, Yaya Mi
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Abstract

Tectono-geochemical analysis is one of the key technical methods for deep prospecting and prediction, but the extraction of information on weak and low degrees of mineralization remains a significant challenge. This study takes the Maoping super-large germanium-rich lead–zinc deposit in northeastern Yunnan as an example, systematically analyzes the mineralization element assemblages and their anomaly distribution characteristics, extracts information on low and weak anomalies at depth, clarifies the spatial distribution of ore-forming element anomalies and fluid migration patterns, and establishes tectono-geochemical deep anomaly evaluation criteria and prospecting models, thereby proposing directions for deep prospecting in the deposit. This research shows that the mineralization element assemblage of the F1 factor (Cd-Cu-Ge-Zn-Sb-In-Pb-Sr(-)-As-Hg) anomalies represents near-ore halos; the element assemblage of the F2 factor (Ni-Co-Cr-Rb-Ga) anomalies represents tail halos; the element assemblage of the F3 factor (Rb-Mo-Tl-As) anomalies represents front halos; and the element assemblage of the F4 factor (Ba-Ga) anomalies represents barite alteration anomalies. Elements such as Zn and Pb exhibit significant anomalies near the lead–zinc ore bodies. In the study area, vertical anomalies in the eastern region of the Luoze River indicate that ore-forming fluids migrated from the SE at depth to the NW at shallower levels, whereas in the western region, ore-forming fluids migrated from the SW at depth to the NE at shallower levels. Thus, the lateral extensions of different ore bodies in the eastern and western regions of the river have been determined. On this basis, tectono-geochemical deep anomaly evaluation criteria for the deposit are established, and directions for deep prospecting are proposed. This study provides scientific value and practical significance for deep prospecting and exploration engineering planning for similar lead–zinc deposits.

构造地球化学弱、低异常深层成矿信息提取——以滇东北茂坪富锗铅锌矿为例
构造地球化学分析是深部找矿预测的关键技术手段之一,但弱矿化和低矿化程度信息的提取仍然是一个重大挑战。以滇东北茂坪超大型富锗铅锌矿为例,系统分析成矿元素组合及其异常分布特征,提取深部低、弱异常信息,厘清成矿元素异常空间分布和流体运移模式,建立构造地球化学深部异常评价标准和找矿模型。提出了矿床深部找矿方向。研究表明,F1因子(Cd-Cu-Ge-Zn-Sb-In-Pb-Sr(-)- as - hg)异常的成矿元素组合表现为近矿晕;F2因子(Ni-Co-Cr-Rb-Ga)异常的元素组合为尾晕;F3因子(Rb-Mo-Tl-As)异常的元素组合为前晕;F4因子(Ba-Ga)异常的元素组合代表重晶石蚀变异常。锌、铅等元素在铅锌矿体附近表现出明显的异常。研究区洛泽河东部垂直异常表明成矿流体在深部由东南向北西向浅层迁移,而在西部则在深部由西南向北东向浅层迁移。从而确定了东、西段不同矿体的横向伸展。在此基础上,建立了矿床深部构造地球化学异常评价标准,并提出了深部找矿方向。该研究对类似铅锌矿的深部找矿和勘探工程规划具有一定的科学价值和现实意义。
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来源期刊
Acta Geochimica
Acta Geochimica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
2.80
自引率
6.20%
发文量
1134
期刊介绍: Acta Geochimica serves as the international forum for essential research on geochemistry, the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth‘s crust, its oceans and the entire Solar System, as well as a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. The journal focuses on, but is not limited to the following aspects: • Cosmochemistry • Mantle Geochemistry • Ore-deposit Geochemistry • Organic Geochemistry • Environmental Geochemistry • Computational Geochemistry • Isotope Geochemistry • NanoGeochemistry All research articles published in this journal have undergone rigorous peer review. In addition to original research articles, Acta Geochimica publishes reviews and short communications, aiming to rapidly disseminate the research results of timely interest, and comprehensive reviews of emerging topics in all the areas of geochemistry.
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