Natural annealing of Pleochroic haloes in biotite samples from deep drill holes, Fenton Hill, New Mexico
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v008/i005/GL008i005p00501/GL008i005p00501.pdf
Reference13 articles.
1. Albright , J. N. Temperature measurements in the Precambrian section of geothermal test hole no. 2: 1975
2. Influence de la chaleur sur la coloration des halos leochroiques dans la biotite;Deutsch;Il Nuovo Cimento,1960
3. Coloration of biotites by α particles in pleochroic haloes II;Deutsch;Il Nuovo Cimento,1959
4. Pleochroic haloes and the artificial coloration of biotites by α particles;Deutsch;Il Nuovo Cimento,1957
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1. Radiation-damage methods of geochronology and thermochronology;Geochronology and Thermochronology;2017-11-24
2. Reaction aureoles around uraninites within biotite and plagioclase: evidence of low-temperature sequential fluid alteration and LREE-mobilization from monazite;Mineralogical Magazine;2016-06
3. Paleomagnetism and rock magnetism of Quaternary volcanic rocks and Late Paleozoic strata, VC-1 core hole, Valles Caldera, New Mexico, with emphasis on remagnetization of Late Paleozoic strata;Journal of Geophysical Research;1988
4. Constraints on the age of heating at the Fenton Hill Site, Valles Caldera, New Mexico;Journal of Geophysical Research;1986
5. Differential helium retention in zircons: Implications for nuclear waste containment;Geophysical Research Letters;1982-10
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