Members of the Geochronology Lab use a laser or a furnace to melt grains of rock and release argon gas, which they can date using a mass spectrometer and the 40-argon/39-argon dating technique. They use this method to solve geological and geophysical mysteries in Alaska and elsewhere, including the eruptive history of Alaska’s volcanoes, the rate of uplift of Alaska’s mountains, and the tectonic history of Alaska and Russia. Lab users have dated fragments of stone-age tools in an attempt to find the sources of the tools and ancient trading patterns.

jbenowitz [at] alaska [dot] edu (Email)
Primary Services
Includes: muscovite, biotite, hornblende, plagioclase, potassium feldspar, glass and XRF of feldspar separate for K/Ca ratio.
Of note, sample separation cost is included in heating experiment costs and no discount for pure separated mineral aliquots (but appreciated).
Includes: Single mineral phase heating experiments (multiple runs if needed), sample
preparation, irradiation costs, data reduction, digital report, and publication quality figures on request.
Includes: ~10 single grain fusions, sample preparation, irradiation costs, data reduction, digital report, and publication quality figures on request. In addition we will provide a statistically analysis of peak populations of the produced data.
Includes: ~100 single grain fusions, sample preparation, irradiation costs, data reduction, digital report, and publication quality figures on request. In addition we will provide a statistically analysis of peak populations of the produced data.
Includes: Single mineral phase heating experiments (multiple runs), sample
preparation, irradiation costs, data reduction, digital report, and publication quality figures on request. We also include a single Laser incremental 40Ar/39Ar heating experiment (~8 to ~10 steps) on potassium feldspar samples to “predetermine if the sample is a good candidate for furnace isothermal-step heating experiments. We prefer
collaborations on potassium feldspar samples because of the amount of work involved. We will derive thermal history models (Time-temperature) from the analysis.

jbenowitz [at] alaska [dot] edu (Email Jeff)
paul [dot] layer [at] gi [dot] alaska [dot] edu (Email Paul)

UAF College of Natural Science and Mathematics http://www.uaf.edu/cnsm/
UAF Geology Department http://www.uaf.edu/geology/