Research paperNew methods of regional exploration for blind mineralization: Application in the USSR
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Cited by (58)
Application of optically stimulated luminescence in volcanic hydrothermal uranium deposits in the Guyuan Basin, North China
2022, Journal of Geochemical ExplorationCitation Excerpt :Thus, exploration urgently needs new technical methods to find concealed mineral deposits. At the end of the 20th century, various new approaches were introduced to extract anomalies in diverse regolith-covered terrains, such as electrogeochemical (Antropova et al., 1992; Dai et al., 2015), biogeochemical (Özdemir, 2005; Anand et al., 2007), mobile metal ion (Wang et al., 1997; Gray et al., 1999), enzyme leaching (Yeager et al., 1998; Williams and Gunn, 2002) and geogas methods (Wang et al., 1997; Ye et al., 2004). The general characteristics of these methods are capable of detecting signals directly generated from deep ore bodies, exploring several hundred meters in depth and weak signals but reliably, so they are called deep penetration geochemistry (Xie and Wang, 1991; Wang et al., 1999).
Geochemical studies of snow over mineral accumulations under conditions of their overlap by sedimentary rocks of the platform cover
2022, Journal of Geochemical ExplorationCharacteristics of particles in groundwater and their prospecting significance for the Shijiangshan Pb-Zn-Ag deposit, Inner Mongolia, China
2020, Journal of Geochemical ExplorationAssessing geochemical anomalies using geographically weighted lasso
2020, Applied GeochemistryCitation Excerpt :The processes, whether primary or secondary, can involve multiple factors with different physical and chemical properties, and can take place over a wide range of spatial and temporal scales (Cheng, 2012). In addition, the dispersion of geochemical elements can occur in multiple directions, and the driving forces and migration mechanisms can be diverse, leading to complexity in the distribution of geochemical patterns (e.g., Kristiansson, 1982; Clark et al., 1990; Antropova et al., 1992; Wang et al., 1997; Mann et al., 1998; Cameron et al., 2002, 2004). For example, Yousefi et al. (2019) classified the factors acting as critical controls on the mineral system into three categories: pre–, syn–, and post–mineralization subsystems.
Nanoparticles in groundwater of the Qujia deposit, eastern China: Prospecting significance for deep-seated ore resources
2020, Ore Geology ReviewsCitation Excerpt :Exploration for deep-seated mineral resources is challenging (Butt and Hough, 2009; Anand et al., 2016). Various methods have been employed to explore for concealed ore deposits, including primary and secondary geochemical halos, stream sediment geochemistry, mobile metal ions, enzyme leaching, leaching of mobile forms of metal in overburden, geogas, electrogeochemistry, biogeochemistry, and hydrochemistry (Kristiansson and Malmqvist, 1982; Butt and Gole, 1985; Cohen et al., 1987; Clark et al., 1990; Antropova et al., 1992; Mann et al., 1998; Luo et al., 1999; Malmqvist et al., 1999; Cameron et al., 2004; de Caritat et al., 2005; Kelley et al., 2006; Anand et al., 2007; Wang et al., 2008; Koplus et al., 2009; Leybourne and Cameron, 2010; Leslie et al., 2013; Wang, 2015; Yilmaz et al., 2015; Gray et al., 2018; Noble et al., 2018). These methods each have specific advantages for the analysis of different near-surface media (e.g., gas, soil, rock, organisms and groundwater).
Deep-penetrating geochemistry for concealed sandstone-type uranium deposits: A case study of Hadatu uranium deposit in the Erenhot Basin, North China
2020, Journal of Geochemical ExplorationCitation Excerpt :Thick transported cover and/or deeply profiles have led to the inability of traditional ore-genetic models and radiometric methods to effectively detect target zones (Wang et al., 2016), leading to serious lags in the exploration of these concealed deposits in the last century. During the last few years, with the introduction and application of the ‘deep-penetrating geochemistry’ method, including geogas method (Lippmann-Pipke et al., 2011; Lu et al., 2019; Wang et al., 1995), enzyme leaching (Clark, 1993; Williams and Gunn, 2002), mobile metal ion (Gray et al., 1999), sequential leaching of mobile forms of metals in overburden (Khoeurn et al., 2019; Wang, 1998), electro- and bio-geochemical methods (Antropova et al., 1992; Ozdemir, 2005), the exploration of sandstone-type uranium deposits has made substantial progress (Uvarova et al., 2012; Wang et al., 2011; Wang et al., 2016). Considerable theoretical and experimental studies have shown that radon (Rn) can penetrate the overburden above the orebody to the surface and form a high anomalous halo (e.g., Fleischer and Mogro-Campero, 1979; Gingrich, 1984; Wang, 2003).