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Journal of Volcanology and Geothermal Research 48 3—4: Removal of the feldspar-derived luminescence component from polymineral fine silt samples for optical dating applications: Tooth, Assessing the reproducibility and accuracy of optical dating of fluvial deposits, Quat.

Implications for dose rate determinations, Radiat.

Scientists can date the age of the tree by counting and measuring the rings. Sources of variability, Radiat. Journal of Volcanology and Geothermal Research 74 3—4: Thermo-luminescence measurements on shock-metamorphosed sandstone and dolomite from Meteor Crater, Arizona.

Journal of Geophysical Research-Planets E1: Van den haute, Investigations on the origin of the equivalent dose distribution in a Dutch coversand, Radiat.

Luminescence dating as a diagnostic criterion for the recognition of Quaternary impact craters.

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Properties of the red TL peak of quartz relevant to thermo-luminescence dating. Dating volcanic and related sediments by luminescence methods: The total absorbed radiation dose is determined by exciting, with light, specific minerals usually quartz or potassium feldspar extracted from the sample, and measuring the amount of light emitted as a result.

Anomalous fading of thermoluminescence in mineral samples. Red thermoluminescence RTL in volcanic quartz: Stokes, Identification of partial resetting using De as a function of illumination time, Radiat.

Monte Carlo modelling and experimental validation, Radiat. The radiation causes charge to remain within the grains in structurally unstable "electron traps". Radiation Measurements 27 2: Thompson, Simulations of thermally transferred OSL signals in quartz: Studies of an artificially shock-loaded H-group chondrite.

Nuclear Tracks and Radiation Measurements 18 1—2: Journal of the Chinese Ceramic Society 32 7: Aitken, Beta and gamma gradients, Nuclear tracks, 10 A rapid measure for testing the dominance of the fast component in the initial OSL signal from quartz, Radiat.

Luminescence Dating: Basic Approach to Geochronology

Roberts, Origin of dose distributions in fluvial sediments, and the prospect of dating single grains from fluvial deposits using optically stimulated luminescence, Radiat. Quaternary Science Reviews 23 5—6: Most luminescence dating methods rely on the assumption that the mineral grains were sufficiently "bleached" at the time of the event being dated.

The photons of the emitted light must have higher energies than the excitation photons in order to avoid measurement of ordinary photoluminescence. Radiation Measurements 42 2: Implications for interpretation of dose-response curves, Radiat.

Geophysical Research Letters 19 Teaching Spanish in Institutions of Higher Learning. Bulletin of Volcanology 64 6: Key topics include the history of environmental systems and life on earth, the discovery of biotic evolution, ecological change, and climate change.

Shock dependence of thermo-luminescence properties. Wintle, Sensitisation and stability of quartz OSL: Singhvi, Distribution in SAR palaeodoses due to spatial heterogeniety of natural beta dose. Roberts, Stochastic modelling of multi-grain equivalent dose De distributions: