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A cirkon (U-Th)/He kormeghatározás módszertani alapjai és alkalmazása fiatal (<1 Ma) vulkánkitörések datálására [PDF]
, 2017 Dunkl, István +3 more
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WITHDRAWN: ESR-thermochronometry of the MIZ1 borehole, Tono, Japan
Quaternary GeochronologyG.E. King +7 more
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Laser microprobe (U-Th)/He thermochronometry of monazite
, 2016 Boyce, J +4 more
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Multi-OSL-thermochronometry of feldspar
Quaternary Geochronology, 2016Abstract Optically stimulated luminescence (OSL)-thermochronometry has recently been proposed as a tool capable of resolving cooling histories from the top 1–2 km of the Earth's crust. This is beyond the resolution of most low-temperature thermochronometric systems, and it offers a new opportunity to investigate the interactions between climate ...
Benny Guralnik
exaly +3 more sources
OSL-thermochronometry using bedrock quartz: A note of caution
Quaternary Geochronology, 2015Abstract Optically stimulated luminescence (OSL) thermochronometry is an emerging application, whose capability to record sub-Million-year thermal histories is of increasing interest to a growing number of subdisciplines of Quaternary research. However, several recent studies have encountered difficulties both in extraction of OSL signals from ...
Benny Guralnik, Markus Waelle
exaly +5 more sources
4He/3He Thermochronometry: Theory, Practice, and Potential Complications
Reviews in Mineralogy and Geochemistry, 2005Thermochronometry most often involves the determination of a cooling age from parent and daughter abundances within an entire crystal or population of crystals (Dodson 1973). Complementary information exists in the spatial concentration distribution of the daughter, C ( x,y,z ), within a single crystal.
David L Shuster
exaly +2 more sources
Northward migration of the eastern Himalayan syntaxis revealed by OSL thermochronometry
Science, 2016Unlinking erosion from uplift in TibetConventional wisdom suggests that the locations of gorges or “knickpoints” along the edges of large plateaus remain fixed because erosion drives tectonic uplift. Nowhere should this be more evident than the rapidly uplifting and eroding Tibetan plateau.
Georgina E King +2 more
exaly +3 more sources
Earth and Planetary Science Letters, 2004
Using classical diffusion theory, we present a mathematical technique for the determination of ^4He concentration profiles in minerals. This approach should prove useful for constraining the low-temperature cooling histories of individual samples and for correcting (U–Th)/He ages for partial diffusive loss.
Shuster, David L., Farley, Kenneth A.
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Using classical diffusion theory, we present a mathematical technique for the determination of ^4He concentration profiles in minerals. This approach should prove useful for constraining the low-temperature cooling histories of individual samples and for correcting (U–Th)/He ages for partial diffusive loss.
Shuster, David L., Farley, Kenneth A.
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Zircon 4He/3He thermochronometry
Geochimica et Cosmochimica Acta, 2015Abstract Multiple thermochronometric methods are often required to constrain time-continuous rock exhumation for studying tectonic processes or development of km-scale topography at Earth’s surface. Here, we explore 4He/3He thermochronometry of zircon as a method for constraining continuous time–temperature (t–T) paths of individual samples through a
Alka Tripathy-Lang +2 more
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