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Tectono-Metallogenesis in Asian Continent
In this part, the main characteristics of the giant ore fields and deposits formed in every tectonic domain will be discussed. This part mainly aims...
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Comparison of the native antimony-bearing Paiting gold deposit, Guizhou Province, China, with Carlin-type gold deposits, Nevada, USA
The Paiting gold deposit, Guizhou Province, China, has been regarded as a Carlin-type gold deposit by several researchers. Alteration and ore-related...
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Introduction
The consumption of primary raw materials has increased ever faster in recent decades, not least due to rapid economic growth in countries such as...
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Mineral Resources in Egypt (I): Metallic Ores
Mineral resources in Egypt are diverse. This chapter deals with the metallic ores. The chapter starts with the iron ores in Egypt and special...
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Early Cretaceous Post-Collisional Collapse of the Yidun Terrane: Geochronological and Geochemical Constraints from Calc-alkaline to Alkaline Basalts in **qiu Area, Southwest China
Several Cretaceous Carlin-like or hydrothermal gold deposits along the Garze-Litang suture zone and Early Cretaceous hydrothermal copper...
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Indirect Associations Between Lamprophyres and Gold-Copper Deposits
This Chapter describes the spatial association between lamprophyres and orogenic gold deposits worldwide. The spatial relationships between...
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The Krásná Hora, Milešov, and Příčovy Sb-Au ore deposits, Bohemian Massif: mineralogy, fluid inclusions, and stable isotope constraints on the deposit formation
The Krásná Hora-Milešov and Příčovy districts (Czech Republic) are the unique examples of Sb-Au subtype orogenic gold deposits in the Bohemian...
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Mineral Resource Exploration
This chapter is concerned with the process of analyzing an area to find mineral deposits, which is termed mineral resource exploration. The...
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Seasonal variability of 7Be in suspended sediments from the Copper River, Alaska: implications for quantifying recent flood deposits in coastal environments
Over the past three decades, particle-reactive cosmogenic 7 Be (t 1/2 = 53.3 d) has frequently been used to quantify recent fluvial sediment inputs to...
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Sulfur isotope and trace element systematics of zoned pyrite crystals from the El Indio Au–Cu–Ag deposit, Chile
We present a comparative study between early, massive pyrite preceding (Cu–Ag) sulfosalt mineralization in high-temperature feeder zones (‘early...
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How Do Mineral Deposits Form and Transform? A Systematic Approach
Formation and transformation of mineral deposits are interactions of geospheresGeosphere , one including the atmosphere, hydrosphere, biosphere,...
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Criteria for the detection of hydrothermal ecosystem faunas in ores of massive sulfide deposits in the Urals
The ore-formational, ore-facies, lithological, and mineralogical-geochemical criteria are defined for the detection of hydrothermal ecosystem fauna...
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Geochemical anomaly separation by multi-fractal modeling: case study of Zarshuran gold deposit
Geochemical anomaly separation, using concentration–area method at Zarshuran Au–As deposit, NW Iran, is studied in this work. Lithogeochemical...
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Dualistic distribution coefficients of trace elements in the system mineral–hydrothermal solution. III. precious metals (Au and Pd) in magnetite and manganmagnetite
Distribution coefficients D of Au and Pd between magnetite (manganmagnetite) and ammonium chloride hydrothermal solution and the structural D ...
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Metallic Mineral Resources in the Twenty-First Century: II. Constraints on Future Supply
Supplying worldwide demand of metallic raw materials throughout the rest of this century may require 5–10 times the amount of metals contained in...
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Problems in estimation of the formation depth of hydrothermal deposits by data on pressure of mineralizing fluids
In this paper, the formation depth of hydrothermal deposits is proposed to be roughly estimated by data on pressure variations in fluid inclusions...
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Fluid inclusion, siliceous rock geochemistry of Shewushan lateritic gold deposit, Hubei Province, eastern China: Implication for the genesis of primary orebody
The Shewushan gold deposit is located 16 km southwest of Jiayu County, Hubei Province, eastern China, which is the largest lateritic gold deposit in...
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Magma-Evaporite-Hydrothermal Metal Associations
Metalliferous fluid indicators and ore deposits due to direct and indirect interactions between magma and evaporites at a regional scale are neither...
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Sources of high-pressure fluids involved in the formation of hydrothermal deposits
Available fluid inclusion data on hydrothermal deposits, deep-seated xenoliths, magmatic and metamorphic rocks were used to generalize the...
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Lithologically controlled invisible gold, Yukon, Canada
The newly discovered Cretaceous Coffee orogenic gold deposit (>4 Moz resource) consists of an extensive oxidised zone developed on primary sulphidic...
