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Preface | |
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Acknowledgements | |
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Nucleosynthesis and nuclear decay | |
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The chart of the nuclides | |
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Nucleosynthesis | |
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Stellar evolution | |
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Stages in the nucleosynthesis of heavy elements | |
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Radioactive decay | |
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Isobaric decay | |
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Alpha- and heavy-particle decay | |
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Nuclear fission and the Oklo natural reactor | |
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The law of radioactive decay | |
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Uniformitarianism | |
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References | |
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Mass spectrometry | |
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Chemical separation | |
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Rb-Sr | |
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Sm-Nd | |
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Lu-Hf | |
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Lead | |
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Ion sources | |
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Thermal ionisation | |
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Plasma-source mass spectrometry | |
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Mass fractionation | |
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Magnetic-sector mass spectrometry | |
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Ion optics | |
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Detectors | |
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Data collection | |
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Isotope dilution | |
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Analysis technique | |
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Double spiking | |
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Applications of MC-ICP-MS to radiogenic isotopes | |
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Hf-W | |
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Lu-Hf | |
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U-Th | |
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Pb-Pb | |
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U-Pb | |
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Sm-Nd | |
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Isochron regression-line fitting | |
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Types of regression fit | |
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Regression fitting with correlated errors | |
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Errorchrons | |
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Dealing with errorchrons | |
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References | |
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The Rb-Sr method | |
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The Rb decay constant | |
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Dating igneous rocks | |
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Sr model ages | |
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The isochron diagram | |
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Erupted isochrons | |
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Meteorite chronology | |
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Dating metamorphic rocks | |
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Open mineral systems | |
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Blocking temperatures | |
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Open whole-rock systems | |
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Dating ore deposits | |
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Dating sedimentary rocks | |
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Shales | |
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Glauconite | |
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Seawater evolution | |
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Measurement of the curve | |
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Modelling the fluxes | |
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The effects of Himalayan erosion | |
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References | |
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The Sm-Nd method | |
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Sm-Nd isochrons | |
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Meteorites | |
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Low-grade meta-igneous rocks | |
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High-grade metamorphic rocks | |
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High-grade metamorphic minerals | |
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Nd isotope evolution and model ages | |
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Chondritic model ages | |
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Depleted-mantle model ages | |
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Model ages and crustal processes | |
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Sedimentary systems | |
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Meta-sedimentary systems | |
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Meta-igneous systems | |
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Partially melted systems | |
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The crustal-growth problem | |
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Crustal-accretion ages | |
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Sediment-provenance ages | |
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Archean depleted mantle | |
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Early Archean crustal provinces | |
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Nd in the oceans | |
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Modern seawater Nd | |
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Ancient seawater Nd | |
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Tertiary seawater Nd | |
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Quaternary seawater Nd | |
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References | |
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Lead isotopes | |
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U-Pb isochrons | |
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U-Pb dating of carbonates | |
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U-Pb (zircon) dating | |
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Lead-loss models | |
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Upper intersection ages | |
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Ion-microprobe analysis | |
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Lead 207/206 ages | |
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Inherited zircon | |
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Alternative presentations of U-Pb data | |
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Alternative U-Pb dating materials | |
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Common (whole-rock) Pb-Pb dating | |
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The geochron | |
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Model (galena) ages | |
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The Holmes-Houtermans model | |
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Conformable leads | |
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Open-system Pb evolution | |
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Pb-Pb dating and crustal evolution | |
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Archean crustal evolution | |
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Paleo-isochrons and metamorphic disturbance | |
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Environmental Pb | |
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Anthropogenic Pb | |
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Pb as an oceanographic tracer | |
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Paleo-seawater Pb | |
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References | |
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Isotope geochemistry of oceanic volcanics | |
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Isotopic tracing of mantle structure | |
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Contamination and alteration | |
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Disequilibrium melting | |
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Mantle plumes | |
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Plum-pudding mantle | |
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Marble-cake mantle | |
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The Nd-Sr isotope diagram | |
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Box models for MORB sources | |
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The mantle array and OIB sources | |
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Mantle convection models | |
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Pb isotope geochemistry | |
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Pb-Pb isochrons and the lead paradox | |
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The development of HIMU | |
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The terrestrial Th/U ratio | |
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The upper-mantle [mu] value re-examined | |
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Mantle reservoirs in isotopic multispace | |
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The mantle plane | |
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The mantle tetrahedron | |
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Identification of mantle components | |
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HIMU | |
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EMII | |
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EMI | |
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Kinematic models for mantle recycling | |
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Depleted OIB sources | |
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Island arcs and mantle evolution | |
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Two-component mixing models | |
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Three-component mixing models | |
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References | |
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Isotope geochemistry of continental rocks | |
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Mantle xenoliths | |
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Mantle metasomatism | |
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Crustal contamination | |
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Two-component mixing models | |
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Melting in natural and experimental systems | |
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Inversion modelling of magma suites | |
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Lithospheric mantle contamination | |
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Phenocrysts as records of magma evolution | |
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Petrogenesis of continental magmas | |
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Kimberlites, carbonatites and lamproites | |
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Alkali basalts | |
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Flood basalts | |
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Precambrian granitoids | |
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Phanerozoic batholiths | |
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References | |
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Osmium isotopes | |
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Osmium analysis | |
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The Re-Os and Pt-Os decay schemes | |
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The Re decay constant | |
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Meteorite isochrons | |
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Dating ores and rocks | |
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Os normalisation and the Pt-Os decay scheme | |
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Mantle osmium | |
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Bulk Silicate Earth | |
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Lithospheric evolution | |
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Primitive upper mantle | |
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Enriched plumes | |
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Osmium from the core | |
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Asthenospheric mantle heterogeneity | |
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Petrogenesis and ore genesis | |
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The Bushveld Complex | |
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The Stillwater Complex | |
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The Sudbury Igneous Complex | |
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Flood-basalt provinces | |
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Seawater osmium | |
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Seawater Os isotope evolution | |
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Os fluxes and residence times | |
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References | |
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Lu-Hf and other lithophile isotope systems | |
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Lu-Hf geochronology | |
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The Lu decay constant and the CHUR composition | |
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Dating metamorphism | |
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Mantle Hf evolution | |
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Hf zircon analysis | |
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Archean sediments | |
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Western Greenland | |
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Mantle depletion and recycling | |
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Sediment recycling | |
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Seawater hafnium | |
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The La-Ce and La-Ba systems | |
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La-Ba geochronology | |
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La-Ce geochronology | |
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Ce isotope geochemistry | |
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The K-Ca system | |
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References | |
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K-Ar and Ar-Ar dating | |
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The K-Ar dating method | |
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Analytical techniques | |
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Inherited argon and the K-Ar isochron diagram | |
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Argon loss | |
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The [superscript 40]Ar-[superscript 39]Ar dating technique | |
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[superscript 40]Ar-[superscript 39]Ar measurement | |
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Irradiation corrections | |
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Step heating | |
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Argon-loss events | |
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Excess argon | |
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Dating paleomagnetism: a case study | |
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[superscript 39]Ar recoil | |
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Dating glauconite and clay minerals | |
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Laser-probe dating | |
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Method development | |
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Applications of laser-probe dating | |
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Timescale calibration | |
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The magnetic-reversal timescale | |
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The astronomical timescale | |
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Intercalibration of decay constants | |
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Thermochronometry | |
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Arrhenius modelling | |
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Complex diffusion models | |
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K-feldspar thermochronometry | |
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References | |
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Rare-gas geochemistry | |
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Helium | |
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Mass spectrometry | |
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Helium production in nature | |
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Terrestrial primordial helium | |
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The 'two-reservoir' model | |
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Crustal helium | |
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Helium and volatiles | |
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Helium and interplanetary dust | |
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Neon | |
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Neon production | |
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Solar neon in the earth | |
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Neon and helium | |
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Argon | |
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Terrestrial primordial argon | |
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Neon-argon | |
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Argon-38 | |
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Xenon | |
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Iodogenic xenon | |
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Fissiogenic xenon | |
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Solar xenon | |
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References | |
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U-series dating | |
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Secular equilibrium and disequilibrium | |
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Analytical methods | |
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Mass spectrometry | |
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Daughter-excess methods | |
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[superscript 234]U dating of carbonates | |
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[superscript 234]U dating of Fe-Mn crusts | |
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[superscript 230]Th sediment dating | |
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[superscript 230]Th-[superscript 232]Th | |
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[superscript 230]Th sediment stratigraphy | |
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[superscript 231]Pa-[superscript 230]Th | |
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[superscript 210]Pb | |
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Daughter-deficiency methods | |
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[superscript 230]Th: theory | |
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[superscript 230]Th: applications | |
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[superscript 230]Th: dirty calcite | |
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[superscript 231]Pa | |
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U-series dating of open systems | |
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[superscript 231]Pa-[superscript 230]Th | |
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ESR-[superscript 230]Th | |
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References | |
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U-series geochemistry of igneous systems | |
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Geochronology of volcanic rocks | |
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The U-Th isochron diagram | |
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Ra-Th isochron diagrams | |
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U-series model age dating | |
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Magma-chamber evolution | |
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The Th isotope evolution diagram | |
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Short-lived species in magma evolution | |
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Mantle-melting models | |
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Melting under ocean ridges | |
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The effect of source convection | |
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The effect of melting depth | |
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The effect of source composition | |
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Evidence from short-lived species | |
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Evidence for mantle upwelling rates | |
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Evidence from Th-Sr and Th-U mantle arrays | |
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Evidence for crustal melting and contamination | |
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Sources of continental magmas | |
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Subduction-zone processes | |
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U-Th evidence | |
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Ra-Th evidence | |
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References | |
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Cosmogenic nuclides | |
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Carbon-14 | |
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[superscript 14]C measurement by counting | |
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The closed-system assumption | |
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The initial-ratio assumption | |
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Dendrochronology | |
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Production and climatic effects | |
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Radiocarbon in the oceans | |
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The 'Ocean Conveyor Belt' | |
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Accelerator mass spectrometry | |
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Radiocarbon dating by AMS | |
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Beryllium-10 | |
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[superscript 10]Be in the atmosphere | |
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[superscript 10]Be in soil profiles | |
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[superscript 10]Be in snow and ice | |
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[superscript 10]Be in the oceans | |
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Comparison of [superscript 10]Be with other tracers | |
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[superscript 10]Be in magmatic systems | |
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Chlorine-36 | |
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Iodine-129 | |
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In situ cosmogenic isotopes | |
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Al-26 meteorite exposure ages | |
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Al-Be terrestrial exposure ages | |
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Chlorine-36 exposure ages | |
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References | |
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Extinct radionuclides | |
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Production and decay | |
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Extant actinides | |
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Xenon isotopes | |
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I-Xe | |
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Pu-Xe | |
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I-Xe chronology | |
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Very-short-lived species | |
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Al-Mg | |
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Ca-K | |
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Be-10 | |
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Short-lived species in planetary differentiation | |
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Pd-Ag | |
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Mn-Cr | |
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Fe-Ni | |
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Hf-W | |
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[superscript 146]Sm-[superscript 142]Nd | |
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Absent species | |
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Cm-U | |
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Conclusions | |
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References | |
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Fission-track dating | |
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Track formation | |
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Track etching | |
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Counting techniques | |
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The population method | |
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The external-detector method | |
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Re-etching and re-polishing | |
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Detrital populations | |
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Track annealing | |
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Uplift and subsidence rates | |
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Track-length measurements | |
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Projected tracks | |
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Confined tracks | |
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Pressure effects | |
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References | |
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Index | |