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Re-Os Isotope Geochemistry of Magmatic Sulfide Ore Systems
1999Abstract The formation of magmatic Cu-Ni-Co-platinum-group element (PGE) sulfide deposits is dependent on mantlederived silicate magmas (komatiites and basalts) attaining sulfide saturation. Because the sulfur content of the upper mantle is considered to be low (250 ppm; McDonough and Sun, 1995), it is likely that, for moderate to ...
D. D. Lambert +3 more
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High precision Re-Os isotopic dating of molybdenites
Molybdenite is an ideal mineral for Re-Os isotopic dating, and its Re-Os isotopic systematics are widely employed to constrain the timing of hydrothermal metal mineralization.Xiaorui Fan +4 more
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Re-Os Isotope ages of molybdenum deposits in East Qinling and their significance
Chinese Journal of Geochemistry, 1995Dating of metallic ore deposits has been one of the problems concerned with by ore geologists for many years. The establishment of the Re-Os Isotope Laboratory at the Institute of Rock and Mineral Analysis, Chinese Academy of Geological Sciences, has provided us with a new technique to carry out geochronological studies of molybdenum ores.
Dianhao Huang +3 more
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Application of Re-Os isotopes to the study of lithospheric processes in Archaean terrains
2021This thesis was scanned from the print manuscript for digital preservation and is copyright the author. Researchers can access this thesis by asking their local university, institution or public library to make a request on their behalf. Monash staff and postgraduate students can use the link in the References field.
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Economic Geology, 2012
The Lala Fe-Cu deposit in the Kangdian iron oxide copper-gold (IOCG) metallogenic province, SW China, is hosted in the Paleoproterozoic Hekou Group. This volcanic-sedimentary sequence has undergone upper greenschist-lower amphibolite facies metamorphism at ~850 Ma.
Chen, WT, Zhou, MF
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The Lala Fe-Cu deposit in the Kangdian iron oxide copper-gold (IOCG) metallogenic province, SW China, is hosted in the Paleoproterozoic Hekou Group. This volcanic-sedimentary sequence has undergone upper greenschist-lower amphibolite facies metamorphism at ~850 Ma.
Chen, WT, Zhou, MF
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Application of the Pt–Re–Os isotopic systems to mantle geochemistry and geochronology
Lithos, 2005Abstract The Re–Os system has now been applied to a wide variety of problems in the solid earth sciences. This review concentrates on applications of the Re–Os system to understanding the age and composition of the mantle and the role that various materials in the mantle play in generating surface magmas.
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Enriched Pt-Re-Os Isotope Systematics in Plume Lavas Explained by Metasomatic Sulfides
Science, 2008To explain the elevated osmium isotope ( 186 Os- 187 Os) signatures in oceanic basalts, the possibility of material flux from the metallic core into the crust has been invoked. This hypothesis conflicts with theoretical constraints on Earth's thermal and dynamic history.
Ambre, Luguet +6 more
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Evolution of the Earth's Mantle: Perspective from the Re-Os Isotopic System
Mineralogical Magazine, 1994The Re-Os isotopic system (Allegre and Luck, 1980; Faure, 1986; Shirey, 1991) has seen increasing use as a unique tracer, complementry to other radioisotope systems because of its chaleophile/siderophile behavior. Increased use has followed improvements in measurement sensitivity (Creaser et al., 1991; Vlkening et aL, 1991), analytical accuracy ...
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Re-Os Isotopic Characteristics of Himalayan River Sediments and Source Rocks
Mineralogical Magazine, 1998The 187Os/188Os ratio of the oceans has increased markedly during the Cenozoic Era, particularly during the past 15 My (Pegram et al., 1992; Peucker-Ehrenbrink et al., 1995). Some authors attribute this rise to increased weathering caused by the Himalayan collision, in analogy with similar models proposed to explain the seawater Sr isotopic record.
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Interpretation of geological significance of Re-Os isotopic age of bitumen
Acta Petrologica Sinica, 2022LI Chao +7 more
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