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TitleCharacterization of helium release from apatite by continuous ramped heating
 
AuthorIdleman, B D; Zeitler, P K; McDannell, K TORCID logo
SourceChemical Geology vol. 476, 2017 p. 223-232, https://doi.org/10.1016/j.chemgeo.2017.11.019
Image
Year2017
Alt SeriesNatural Resources Canada, Contribution Series 20180056
PublisherElsevier BV
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf; html
Subjectsgeochronology; radiometric dating; fission-track dates; helium isotopes; apatite; thermal analyses; mass spectrometer analysis; Methodology
Illustrationsgraphs
ProgramGEM2: Geo-mapping for Energy and Minerals TransGEM
Released2017 11 17
AbstractKnowledge of the kinetic behavior of He in apatite and other U- and Th-bearing minerals comes largely from detailed step-heating experiments, yet such experiments are time consuming and are rarely performed during routine thermochronological studies using the U-Th/He method. We propose a new analytical method for measuring both the bulk 4He abundance and the kinetics of He release in apatite. Using this method He is extracted from samples by continuous heating using a ramped temperature schedule under static vacuum conditions, and the evolved He is measured periodically as it accumulates in the extraction system. Continuous ramped heating (CRH) experiments can be conducted using instrumentation available in most noble-gas thermochronology labs but require particular attention to temperature control, measurement linearity and dynamic range, and suppression of active gases co-evolved with He. CRH experiments require little more time than conventional single-step heating measurements but yield a detailed record of He release not provided by conventional methods. Kinetic parameters for He diffusion in Durango apatite derived from continuous heating data agree well with those obtained from published step-heating studies. The continuous record of He release obtained from CRH experiments also provides important information about the siting of He and the presence of multiple He components in apatite, some of which may be responsible for anomalous U-Th/He ages and high age dispersion. As such the CRH method shows promise as a useful sample screening tool for apatite U-Th/He thermochronology.
Summary(Plain Language Summary, not published)
Age dispersion is a common and perplexing problem in apatite U-Th/He thermochronology, particularly for old, slowly cooled grains. Conventional total-gas heating experiments on replicates help to identify misbehavior but shed little light on the causes of dispersion. We are exploring this problem using a new analytical method whereby apatite crystals are subjected to a continuous ramped heating (CRH) schedule and the evolved He is accumulated and measured continuously by static mass spectrometry. Moreover, the method offers the opportunity to obtain sample-specific kinetic data for every sample. CRH analyses can be performed using most of the instrumentation available in noble-gas laboratories, but the method requires careful temperature control, effective mitigation of coevolved gases, and precise characterization of mass spectrometer sensitivity.
GEOSCAN ID308251

 
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