Results 281 to 290 of about 2,041,224 (354)
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2020
Gold mineralization potential of Mongolia has been studied since the 1900s, and small-scale mining activities have been known in the Northern Khentii metallogenic zone of Mongolia. Based on joint Mongolian-Russian, Mongolian-Japanese, and European gold explorers, seven metallogenic belts are recognized: (1) Mongol-Altai, (2) Nuur, (3) Northern Mongolia,
Gunchin Dejidmaa, Uyanga Bold
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Gold mineralization potential of Mongolia has been studied since the 1900s, and small-scale mining activities have been known in the Northern Khentii metallogenic zone of Mongolia. Based on joint Mongolian-Russian, Mongolian-Japanese, and European gold explorers, seven metallogenic belts are recognized: (1) Mongol-Altai, (2) Nuur, (3) Northern Mongolia,
Gunchin Dejidmaa, Uyanga Bold
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ACS Earth and Space Chemistry, 2019
Carlin-style (sediment-hosted, “invisible” gold) and epithermal gold deposits are commonly enriched in mercury (Hg), but the source of this metal is not well-known.
R. Yin +10 more
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Carlin-style (sediment-hosted, “invisible” gold) and epithermal gold deposits are commonly enriched in mercury (Hg), but the source of this metal is not well-known.
R. Yin +10 more
semanticscholar +1 more source
Electrolytic Gold Deposition on Dodecanethiol-Modified Gold Films
Langmuir, 2009The electrochemical nucleation and growth of Au from a Au sulfite electrolyte onto dodecanethiol-modified Au surfaces is investigated by a combination of microscopy and chronoamperometry methods. The self-assembled dodecanethiol monolayers are continuous but exhibit defects in correspondence of the Au grain boundaries and on top of Au terraces ...
Gyana, Pattanaik +3 more
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Economic Geology, 1970
Studies of fresh carbonate host rocks and unoxidized gold ores of the Carlin mine indicate that gold, quartz, barite, pyrite, and other sulfides were introduced into the Roberts Mountains Formation by acid hydrothermal solutions. Laboratory investigations on the carbonaceous materials in the host rocks and ores and studies of reactions between ...
Arthur S. Radtke, Bernard J. Scheiner
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Studies of fresh carbonate host rocks and unoxidized gold ores of the Carlin mine indicate that gold, quartz, barite, pyrite, and other sulfides were introduced into the Roberts Mountains Formation by acid hydrothermal solutions. Laboratory investigations on the carbonaceous materials in the host rocks and ores and studies of reactions between ...
Arthur S. Radtke, Bernard J. Scheiner
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Transactions of the IMF, 1996
A uniform, bright, high purity gold deposit can be obtained by using a dip gold plating process, characterized by high bath stability. The properties of the deposit have been examined by SEM, SRD and XPS.
Han Keping, Fang Jingli
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A uniform, bright, high purity gold deposit can be obtained by using a dip gold plating process, characterized by high bath stability. The properties of the deposit have been examined by SEM, SRD and XPS.
Han Keping, Fang Jingli
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Metallogenetic model of Jiaodong-type gold deposits, eastern China
Science China. Earth Sciences, 2023Jun Deng +8 more
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Laser-induced deposition of gold
AIP Conference Proceedings, 1986AbstractThe laser-induced, vapor-phase deposition of gold metal from dimethyl-(2,4-pentanedionato) gold (III) and two fluorinated derivatives was examined by both photopyrolytic (LCVD) and photochemical modes of decomposition. High purity gold deposits are formed by LCVD with the rates of deposition being extremely vapor pressure dependent and thus ...
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The big mantle wedge and decratonic gold deposits
Science China. Earth Sciences, 2021R. Zhu, Wei-dong Sun
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Journal of Electroanalytical Chemistry and Interfacial Electrochemistry, 1974
Summary It is shown that in the case of Au deposition from CN− solution slow surface area changes take place which can be observed by potentiostatic pulse and a.c. impedance methods. The mechanism of incorporation of CN into the Au deposit is briefly discussed.
I.R. Burrows, J.A. Harrison, J. Thompson
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Summary It is shown that in the case of Au deposition from CN− solution slow surface area changes take place which can be observed by potentiostatic pulse and a.c. impedance methods. The mechanism of incorporation of CN into the Au deposit is briefly discussed.
I.R. Burrows, J.A. Harrison, J. Thompson
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