PWNx̃[~ PXNx̃[~ QONx̃[~ QPNx̃[~


12 13@K Condomines et al., Timescales of magma chamber processes and dating of young volcanic rocks
12 8@쑺׎m Guehther et al., Slab window migration and terrane accretion preserved by low-temperature thermochronoogy of a magmatic arc, northern Antarctic Peninsula
12 2@ѐL Millard and Hedges, A diffusion-absorption model of uranium uptake by archaeological bone
1117@ΐVV Gogen and Wagner, Alpha-recoil track dating of Quaternary volcanics
114@_q Hashimoto et al., Blue and red thermoluminescence of natural quarts in the temperature region from -196 to 400°C


Dill, Can REE patterns and U-Th variations be used as a tool to determine the origin of apatite in clastic rocks?


Thomsen et al., Luminescence response to irradiation using mini X-ray generators


Berger, Thermoluminescence dating of volcanic ash


Green, On the thermo-tectonic evolution of Northern England: evidence from fission track analysis


Hunphreys, Grain and subgrain characterization by electron backscatter diffraction


Frechen and Dodonov, Loess chronology of the Middle and Upper Pleistocene in Tajikistan


Ishidera et al., Investigation of montmorillonite alternation and form of iron corrosion products in compacted bentonite in contact with carbon steel for ten years


Gleadow, Fission-track dating methods: what are the real alternatives?


Toms et al., Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina


Lisker et al., Apatite thermochronology in modern geology


Jolivet et al., Can fossil bones and teeth be dated using fission track analysis?
TPS@_q Forman et al., Luminescence geochronology for sediments from Lake El' gygytgyn, northeast Siberia, Russia: constraing the timing of paleoenvironmental events for the past 200 ka
SQV@Rc_j Wilson et al., The effect of iron monmorillonite stability (II) Experimental investigation
SPX@ɓ[ Grun, The kinetics of TL peaks and its effect on the dose versus temperature plot
SPQ@ΐVV Yamada et al., Assesment of overetching factor for confined track length measurement in zircon