Direct rhenium-osmium age of the oxfordian-kimmidgian boundary, Staffin Bay, Isle of Skye, UK and the Late Jurassic geologic timescale.
(2007)
Journal Article
Selby, D. (2007). Direct rhenium-osmium age of the oxfordian-kimmidgian boundary, Staffin Bay, Isle of Skye, UK and the Late Jurassic geologic timescale
Outputs (5)
Age of and source constraints for the Giant Murantau gold deposit, Uzbekistan, from coupled Re-Os-He isotopes in arsenopyrite. (2007)
Journal Article
Morelli, R., Creaser, R., Seltmann, R., Stuart, F., Selby, D., & Graupner, T. (2007). Age of and source constraints for the Giant Murantau gold deposit, Uzbekistan, from coupled Re-Os-He isotopes in arsenopyrite. Geology, 35, 795-798. https://doi.org/10.1130/g23521a.1
Re-Os elemental and isotopic systematics in crude oils. (2007)
Journal Article
Selby, D., Creaser, R., & Fowler, M. (2007). Re-Os elemental and isotopic systematics in crude oils. Geochimica et Cosmochimica Acta, 71, 378-386. https://doi.org/10.1016/j.gca.2006.09.005
The role and temporal evolution of granite–related molybdenite mineral systems along the Caledonian-Appalachian orogen: Implications from Re-Os geochronology and fluid inclusion microthermometry. (2007)
Journal Article
Feely, M., Selby, D., Conliffe, J., & Judge, M. (2007). The role and temporal evolution of granite–related molybdenite mineral systems along the Caledonian-Appalachian orogen: Implications from Re-Os geochronology and fluid inclusion microthermometry. Applied Earth Science, 116(3), 143-149. https://doi.org/10.1179/174327507x207465Re–Os geochronometry is combined with fluid inclusion microthermometry to investigate the granite molybdenite system associated with the late-Caledonian Omey Granite, Connemara, western Ireland. Molybdenite in the Omey pluton is hosted by thin vertic... Read More about The role and temporal evolution of granite–related molybdenite mineral systems along the Caledonian-Appalachian orogen: Implications from Re-Os geochronology and fluid inclusion microthermometry..
Assessment of the 187Re decay constant by cross calibration of Re–Os molybdenite and U–Pb zircon chronometers in magmatic ore systems (2007)
Journal Article
Selby, D., Creaser, R., Stein, H., Markey, R., & Hannah, J. (2007). Assessment of the 187Re decay constant by cross calibration of Re–Os molybdenite and U–Pb zircon chronometers in magmatic ore systems. Geochimica et Cosmochimica Acta, 71(8), 1999-2013. https://doi.org/10.1016/j.gca.2007.01.008The past decade has seen renewed interest in 187Re–187Os geochronology using a variety of matrices including sulfide minerals, shales and meteorites. The most widely used value of the 187Re decay constant (λ 187Re) is 1.666 ± 0.005 × 10−11 a−1 (±0.31... Read More about Assessment of the 187Re decay constant by cross calibration of Re–Os molybdenite and U–Pb zircon chronometers in magmatic ore systems.