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Lasing in the Holocene; extending the super 40 Ar- super 39 Ar laser probe method into the super 14 C age range.

Hu, Qiang; Smith, Patrick E; Evensen, Norman M; York, Derek (1994) Lasing in the Holocene; extending the super 40 Ar- super 39 Ar laser probe method into the super 14 C age range. Earth and Planetary Science Letters. 123; 1-4, Pages 331-336. 1994.

AuthorsHu, Qiang; Smith, Patrick E; Evensen, Norman M; York, Derek
Year1994
TitleLasing in the Holocene; extending the super 40 Ar- super 39 Ar laser probe method into the super 14 C age range.
SourceEarth and Planetary Science Letters. 123; 1-4, Pages 331-336. 1994.
PublisherElsevier. Amsterdam, Netherlands. 1994.
Document typeSerial
ISSN0012-821X
GeoRef1994-037732
Keywordsabsolute-age; alkali-feldspar; Ar-Ar; C-14; calibration-; California-; carbon-; Cenozoic-; dates-; east-central-California; feldspar-group; framework-silicates; Holocene-; isochrons-; isotopes-; laser-methods; methods-; Mono-County-California; Mono-Craters; Pleistocene-; Quaternary-; radioactive-isotopes; sanidine-; silicates-; United-States; upper-Pleistocene
DOI10.1016/0012-821X(94)90277-1

Abstract

Dating methods applicable to the last 50,000 yr, such as super 14 C, require absolute calibrations, which are difficult to obtain over much of this interval. Extension of the super 40 Ar- super 39 Ar isochron technique to ages <50,000 yr would make this well-understood absolute dating method available for calibration of cosmic-ray-dependent methods and for dating of young materials not suitable for super 14 C dating. We have dated the Mono craters, California, at 12,560+ or -470 yr, using laser fusion to generate an isochron from 63 sanidine crystals from 5 sites. The near-atmospheric initial isotopic ratios and the agreement in ages from all sites suggest that no significant excess argon is present. It thus appears that, particularly with improved instrumentation and techniques currently under development, most of the super 14 C age range is accessible to super 40 Ar- super 39 Ar laser dating.

5 samples from this reference

SampleRock nameMajorTraceIsotope
5G203Rhyolite
5G204Rhyolite
6G007Rhyolite
75M005Rhyolite
5G201Rhyolite