2015
DOI: 10.1016/j.gexplo.2015.07.007
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TEM observations of particles based on sampling in gas and soil at the Dongshengmiao polymetallic pyrite deposit, Inner Mongolia, Northern China

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Cited by 27 publications
(7 citation statements)
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References 35 publications
(60 reference statements)
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“…Since Kristiansson and Malmqvist proposed the existence of naturally occurring gas ascending from the Earth's interior (Kristiansson & Malmqvist, , , ), researchers have confirmed ascending gas occurring in many places (e.g., Cao, ; Cao, Hu, et al, ; Cao, Hu, Liang, & Peng, ; Cao, Li, Jiang, & Hu, ; Cao, Liu, Xiong, & Qin, ; Etiope & Ciccioli, ; Luo, Cao, Yan, & Yi, ; Malmqvist, Kristiansson, & Kristiansson, ; Wang, Cao, Lin, & Wu, ), especially in seismically active regions (Italiano, D'Alessandro, & Martelli, ; Toutain & Baubron, ). As active faults have high permeability and porosity and can thus act as channels for ascending gas (Etiope, ; Mörner & Etiope, ; Toutain & Baubron, ), ascending gas can move rapidly in dry media (Etiope & Lombardi, , ).…”
Section: Discussionmentioning
confidence: 99%
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“…Since Kristiansson and Malmqvist proposed the existence of naturally occurring gas ascending from the Earth's interior (Kristiansson & Malmqvist, , , ), researchers have confirmed ascending gas occurring in many places (e.g., Cao, ; Cao, Hu, et al, ; Cao, Hu, Liang, & Peng, ; Cao, Li, Jiang, & Hu, ; Cao, Liu, Xiong, & Qin, ; Etiope & Ciccioli, ; Luo, Cao, Yan, & Yi, ; Malmqvist, Kristiansson, & Kristiansson, ; Wang, Cao, Lin, & Wu, ), especially in seismically active regions (Italiano, D'Alessandro, & Martelli, ; Toutain & Baubron, ). As active faults have high permeability and porosity and can thus act as channels for ascending gas (Etiope, ; Mörner & Etiope, ; Toutain & Baubron, ), ascending gas can move rapidly in dry media (Etiope & Lombardi, , ).…”
Section: Discussionmentioning
confidence: 99%
“…In our study, there are many ore‐forming elements (e.g., S, Cl, Cr, Zn, Mn, Ni, Cu, Cd, Sn, Sb, Pt, and Pb) that have been found in particulates caused by the earthquake, indicating that earthquakes can activate ore‐forming elements and cause them to migrate from deep to shallow soil. In addition, ore‐bearing particulates have been found in many deposits (e.g., Cao et al, ; Cheng, Cao, Li, Hu, & Yi, ; Dai, Cao, Lai, & Wu, ; Hu, Cao, Hopke, & Holub, ; Hu, Cao, & Jiang, ; Hu, Cao, Jiang, Wang, & Yi, ; Li, Cao, Ke, Liu, & Wei, ; Luo et al, ; Mi, Cao, Wu, & Wang, ; Wang et al, ). Therefore, although we cannot demonstrate that the ore‐bearing particulates ultimately form ore deposits, they may be an important component of ore deposits, which are formed during an earthquake.…”
Section: Discussionmentioning
confidence: 99%
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“…It was also demonstrated that metal‐bearing particles can transfer upwards through ascending gas flow and ground water (Cao et al, , ; Cao, ; Hu et al, ; Li et al, ). Luo et al () has demonstrated that there were many metal‐bearing particles preserved in the soil above the orebodies. Besides, through a detailed comparison of particles in ascending gas flow samples and soil samples, particles from the two media were both supposed to originate directly from the deep concealed orebodies.…”
Section: Discussionmentioning
confidence: 99%
“…Actually, some studies have found that metal‐bearing particles captured from various media in the surface area of concealed deposits, such as ground soils, ascending gas flows, fault gouges and ground water, can reflect the chemical composition of a concealed orebody and subsequently be used for prospecting deep concealed deposits (Cao et al, , , ; Wei et al, ; Hu et al, , b; Luo et al, ; Li et al, ). Particle analysis can overcome the problems of physiological barriers and detection limit, when compared with element concentration analysis.…”
Section: Introductionmentioning
confidence: 99%