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Research (Crustal Re-Os Geochronology)

Important User Information: Remote access to EBSCO’s databases is permitted to patrons of subscribing institutions accessing from remote locations for personal, non-commercial use. However, remote access to EBSCO’s databases from non-subscribing institutions is not allowed if the purpose of the use is for commercial gain through cost reduction or avoidance for a non-subscribing institution. Source: Mineralium Deposita. Jun, Vol. It consists of lenses of marble, calc-silicate rocks, and skarns.

More recently however, Re/Os dating of arsenopyrite suggests that the vein formation began with the onset of metamorphism circa Ma. Other ages at about.

The Maoling gold deposit, one of the large gold deposits in eastern Liaoning Province, NE China, is an arsenopyrite-disseminated gold deposit with a resource of approximately 25 t Au and an average Au grade of 3. This is a preview of subscription content, log in to check access. Zhou, T. Kong, F. Chen, C. Wang, W. Google Scholar. Dai, L. Gold Geol. Li, X.

Suzuki, K. Stein, H. Frei, R.

Arsenopyrite

Researcher Qu W. Following molybdenite deposits, they innovatively produced standard substance for the Re-Os dating of Cu-Ni alkides and seafloor cobalt-rich crusts, which was certified as a national class 1 standard substance. After modifying the sample selection method, high-temperature sealed dissolution and testing analysis processes, they established the Re-Os isotopic analysis technique and dating method for pyrite, arsenopyrite, limestone, graphite, asphalt and other ultralow Re-Os content series samples.

Their total procedure blank and testing precision are already the international leading level. This offers a new technical approach to the isotopic dating of sedimentary rocks, hydrocarbon source rocks and oil-gas pools. Re-Os isotopic testing.

using Re–Os isotopic dating on single minerals such as pyrite or arsenopyrite from sulfide ores (Morelli and Creaser, ), but Re and. Os concentrations are​.

The Archean-Proterozoic craton of West Africa hosts numerous gold deposits, which are spatially and temporally related to the Eburnean orogeny that took place between and Ma, and included multiple deformation events. The majority of these gold deposits are located along shear zones. The structural history is relatively well established for most gold deposits, but absolute timing of the mineralization is commonly lacking. Gold mineralization was structurally characterized at each deposit, and dated by the Re-Os method on pyrite, arsenopyrite, and pyrrhotite grains that were coeval with the gold deposition.

Combined structural and Re-Os geochronological constraints allow two groups of gold deposits to be distinguished. Early orogenic gold formed during the Eoeburnean orogeny, i. These Re-Os ages on the early sulfides at Wassa and Kiaka are significant because they definitively provide the first direct age constraints on gold-only Eoeburnean mineralization in the Birimian of West Africa.

The high uncertainties on the Nassara and Damang ages may be directly linked to the low rhenium and osmium contents of the studied samples. These results highlight the polyphase character of the widespread gold mineralization in the West African craton.

Top9. Re-Os isotopic analysis opened a new approach to dating sedimentary rocks

This reos is affected by the charge re-os of rhenium atom. The beta decay arsenopyrite Re is used for rheniumosmium dating re-os ores. Facts Re-os Osmium. Uses of osmium. Because of its density, osmium is often alloyed with other precious metals to make products such as instrument pivots, phonograph needles, and electrical.

This reos is affected by the charge re-os of rhenium atom. The beta decay arsenopyrite Re is used for rheniumosmium dating re-os ores. Although our previous.

Degao Zhai, Anthony E. Economic Geology ; 5 : — Native gold is intergrown with molybdenite and pyrite in auriferous quartz veins hosted by a monzogranite-monzonite stock and locally by Proterozoic gneiss, thereby offering an excellent opportunity to directly date the mineralizing event. Uranium-Pb age determinations for zircon yielded ages for the monzogranite and monzonite of Numerous mafic to felsic dikes, which are crosscut by ore veins pre-ore , parallel to these veins possibly synore , or crosscut by them post-ore , were carefully examined and dated.

The age of mineralization was determined directly using the Re-Os method applied to molybdenite. A total of 19 molybdenite samples separated from auriferous quartz veins yielded widely differing Re-Os model ages of to Ma, and replicate analyses of individual samples also yielded widely differing ages. Significantly, the wide range is attributable entirely to the results obtained for some coarse-grained molybdenite samples and is interpreted to be due to Re and Os isotope decoupling, the considerable spatial Re heterogeneity, the analytical procedure e.

Thus, the molybdenite Re-Os ages are identical, within uncertainty, to those of the dikes that are parallel to the ore veins, indicating that these dikes were emplaced contemporaneously with the ore and that they and the Haigou gold mineralization are of late Paleozoic age ca.

Canadian Journal of Earth Sciences

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These results show that arsenic-rich pyrite is called arsenious such as arsenopyrite are potentially very significant (Mumin et al., ), plications (e.g.​, U/Pb dating) and, with the recent advent of multi-collector ICP-MS.

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Mineral deposits of Canada: a synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods; by Goodfellow, W D ed. This publication is contained in Goodfellow, W D; Mineral deposits of Canada: a synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods, Geological Association of Canada, Mineral Deposits Division, Special Publication no. Consolidating Canada’s Geoscience Knowledge.

by the Re-Os method carried out on the pyrites of the host rock. group is dated Ma by the U-Pb method on detrital sulphide; Py, pyrite; Ccp, chalcopyrite; Gn, galena; Sp, sphalerite; Apy, arsenopyrite; Mot.

Rhenium-osmium geochronology using arsenopyrite was undertaken for three gold deposits in the Meguma terrane, Nova Scotia, Canada, in order to better constrain their age of formation and to assess the utility of arsenopyrite for dating similar deposits globally. The lack of common Os in some arsenopyrite samples from both The Ovens and Dufferin permit calculation of single mineral model ages for each deposit, which are identical to those determined using the isochron method.

Initial Os compositions for the two vein types at The Ovens suggest a predominately crustal source of Os in the mineralizing fluids, whereas a less radiogenic initial Os composition for arsenopyrite from Dufferin does not as clearly define a crustal metal source. At a third locality, the Touquoy deposit, the Re-Os systematics of arsenopyrite associated with disseminated gold mineralization do not define a precise formation age, possibly as a result of mixing of Re and Os derived from the mineralizing fluid and the shale host rock.

The Re-Os ages of arsenopyrite indicate that there were at least two distinct periods of gold deposition in the Meguma terrane coinciding with widespread tectonothermal events: regional deformation and metamorphism associated with Acadian orogenesis, and widespread generation of meta- and peraluminous granites and high-grade metamorphism within the basement rocks under the Meguma terrane.

The ca.

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Development of Re-Os geochronology for crustal matrices has been ongoing since in the laboratory. This work has resulted in major advancements in the direct isotopic dating of crustal sulfide minerals, petroleum source-rocks, and natural hydrocarbons, using Re-Os isotopes. For sulfide minerals, Re-Os geochronology has direct application to the timing and duration of hydrothermal ore deposit formation.

arsenopyrite REE characteristics were determined, and. Re–Os dating was used to constrain the age and source material of gold-bearing arsenopyrites from the.

Table S1. It is not known whether environmental O 2 levels increased in a linear fashion or fluctuated dynamically between the evolution of oxygenic photosynthesis and the later Great Oxidation Event. New rhenium-osmium isotope data from the late Archean Mount McRae Shale, Western Australia, reveal a transient episode of oxidative continental weathering more than 50 million years before the onset of the Great Oxidation Event.

Transient oxygenation events, like the one captured by the Mount McRae Shale, probably separated intervals of less oxygenated conditions during the late Archean. Multiple lines of geochemical evidence from sedimentary rocks point to the production and accumulation of photosynthetic O 2 in surface environments since at least 3 billion years ago Ga 1 — 7.

In contrast, sulfur mass-independent fractionation S-MIF indicates that Archean atmospheric O 2 levels were predominantly below 0. However, transiently higher O 2 levels are possible if crustal recycling of S-MIF signatures is taken into account Therefore, evidence for O 2 production during Archean time may represent one of several scenarios. One possibility is that small linear stepwise increases in atmospheric O 2 allowed mild oxygenation and oxidative continental weathering to occur continuously and with increasing intensity in the several hundred million years before the first major accumulation of O 2 in the atmosphere [the ca.

Nonlinear fluctuations in Earth surface redox conditions may have also been driven by variations in the relative fluxes of reducing gases, such as biogenic methane 11 — Distinguishing between these hypotheses is critical for understanding the dynamics of planetary oxygenation on Earth and ultimately the evolution of complex life 7. The 2. Increased Mo and Re concentrations may capture a transient increase in oxidative continental weathering, possibly associated with a rise in atmospheric O 2 levels, and the subsequent decrease in Mo and Re concentrations may reflect a return to a lower redox state 1.

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The Maoling gold deposit is located in the southwestern part of the Liaodong Zircon U–Pb dating of the Wolongquan biotite monzogranite and () obtained an Re–Os isochron age of ± Ma for arsenopyrite in.

The Iso-Kuotko deposit is located 10 km to the north of Suurikuusikko along the same shear zone. Gold mineralization at Iso-Kuotko formed in two major stages: an early stage refractory gold mineralization with auriferous arsenopyrite with similarities to the ore at Suurikuusikko and a late, main stage mineralization with free gold in carbonate-quartz veins with abundant pyrrhotite, native bismuth and other sulphide minerals.

This latter ore is absent at Suurikuusikko. Based on U-Pb dating, as well as Re-Os and Pb-isotope systematics of rock-forming and hydrothermal minerals, we evaluate the relationships between tectonic evolution and formation of gold deposits throughout the late Palaeoproterozoic in the northern part of the CLGB. Results from in situ U-Pb dating of zircon and petrographically well constrained hydrothermal monazite and xenotime by LA-ICPMS, and model age calculations using Re-Os isotopic data for arsenopyrite and in situ Pb-isotope data for galena from the Iso-Kuotko deposit provide evidence for multiple episodes of hydrothermal activity along the KiSZ.

Data suggest coincident felsic magmatism and structurally controlled fluid flow events during wrench fault-dominated N-S shearing associated with early, micro-continent accretion ushering in the Svecofennian orogeny. This time-interval is concurrent with widespread granitoid emplacement at the close of the Svecofennian orogeny. Disturbance of the Re-Os system in the early auriferous arsenopyrite can be connected to the late stage mineralizing processes.

Pb isotope data suggest a mixed mantle and lower crust origin for fluids in the post-orogenic hydrothermal system.

Canadian Journal of Earth Sciences

Technician support will underpin growth of the Program through increased student involvement, increased Front Range collaborations, and expansion of global partnerships. New research opportunities will build on AIRIE’s nine-year history of collaborations with over scientists from industry, government and academia, on projects spanning five continents.

To date, the focus of the Program has been on development, testing, and application of the rhenium-osmium Re-Os molybdenite geochronometer, with transfer of this technology to the mineral industry for application in exploration. Some full text articles may not yet be available without a charge during the embargo administrative interval. Some links on this page may take you to non-federal websites.

by Re–Os dating of a Neoproterozoic, postglacial black shale in Western Chem Geol –87 Martin CE () Re-Os isotopic investigation of the arsenopyrite in Meguma Group gold deposits, Meguma Terrane, Nova Scotia.

Re and Os rhenium and osmium are chalcophile-siderophile elements transition metals with a unique position in isotope geochemistry. Unlike other commonly used decay schemes for radiometric dating, these metals take residency in resource-related media, for example, sulfide minerals, the organic component in black shales, coals, and bitumens and oils. In short, the reducing environment is their haven whereas under oxidizing conditions, Re and Os become unmoored and the radiometric clock becomes compromised.

The clock is not temperature sensitive, and its applicability spans Early Archean to Pleistocene. This Bunsen Medal lecture will explore and review the challenges in bringing Re-Os from the meteorite-mantle community into the crustal environment. At the center of it all is our ability to turn geologic observation into a thoughtful sampling strategy.

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