Results 271 to 280 of about 74,970 (357)
Adsorptive removal of lead from wastewater using pressmud with evaluation of kinetics and adsorption isotherms. [PDF]
Haider B +9 more
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Comparison of dominant foodborne and inhalant allergies developing in the first 5 years of life. [PDF]
Xu Q +7 more
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The turbulent soundscape of intertidal oyster reefs. [PDF]
Volaric MP +5 more
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Reconciling Archean organic-rich mudrocks with low primary productivity before the Great Oxygenation Event. [PDF]
Lotem N +6 more
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Archaean multi-stage magmatic underplating drove formation of continental nuclei in the North China Craton. [PDF]
Liu J +7 more
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U–Pb SHRIMP dating of uraniferous opals
Abstract U–Pb and U-series analyses of four U-rich opal samples using sensitive high-resolution ion microprobe (SHRIMP) demonstrate the potential of this technique for the dating of opals with ages ranging from several tens of thousand years to millions of years.
Nemchin, Alexander +2 more
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Isotopic U–Pb-SHRIMP dating of Mugodzhari eclogites (Kazakhstan)
Доклады Российской академии наук. Науки о Земле / Doklady Earth SciencesIn the extreme south of the Urals, zircons from eclogites and amphibolite were dated in metamorphites of the East Mugodzhar zone. Of the 4 eclogite samples, close (and the most “ancient” – 520±4 million years) concordant age values were obtained in 3 samples, which probably corresponds to the age of the protolith.
K. S. Ivanov
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Contributions to Mineralogy and Petrology, 1999
The potential genetic link between granites and their host sediments can be assessed using zircon age inheritance patterns. In the Lachlan fold belt, southeastern Australia, granites and associated high-grade metasedimentary rocks intrude low-grade Ordovician country rock. This relationship is well-exposed in the Tallangatta region, northeast Victoria (
Keay, S., Steele, D., Compston, W.
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The potential genetic link between granites and their host sediments can be assessed using zircon age inheritance patterns. In the Lachlan fold belt, southeastern Australia, granites and associated high-grade metasedimentary rocks intrude low-grade Ordovician country rock. This relationship is well-exposed in the Tallangatta region, northeast Victoria (
Keay, S., Steele, D., Compston, W.
openaire +4 more sources

