Determining cooling rates from mica 40 Ar/ 39 Ar thermochronology data: Effect of cooling path shape-Reference-Cited by-同舟云学术

Determining cooling rates from mica 40 Ar/ 39 Ar thermochronology data: Effect of cooling path shape

Published:2019-04-23 Issue:3 Volume:31 Page:234-246
ISSN:0954-4879
Container-title:Terra Nova
language:en
Short-container-title:Terra Nova

Author:

McDonald Christopher S.¹²,Warren Clare J.¹^ORCID,Hanke Felix³^ORCID,Chard Julian⁴

Affiliation:

1. School of Environment, Earth and Ecosystem SciencesThe Open UniversityWalton Hall Milton Keynes UK

2. School for Earth and Space ExplorationArizona State University Tempe Arizona

3. Dassault Systèmes Cambridge UK

4. School of Earth and Planetary SciencesThe Institute for Geoscience Research (TIGeR)Curtin University Perth WA Australia

Funder

Natural Environment Research Council

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12390

Reference29 articles.

1. The Effects of Retrograde Reactions and of Diffusion on 40Ar–39Ar Ages of Micas

2. One Hundred Years of Isotope Geochronology, and Counting

3. Closure temperature in cooling geochronological and petrological systems

4. The age of the Keystone Thrust: Laser-fusion40Ar/39Ar dating of Foreland Basin Deposits, southern Spring Mountains, Nevada

5. Advances in 40Ar/39Ar dating: From Archaeology to Planetary Sciences 2017 M. A. Forster G. S. Lister F. Jourdan D. F. Mark C. Verati 40 Ar/ 39 Ar geochronology and the diffusion of 39 Ar in phengite‐muscovite intergrowths during step‐heating experiments in vacuo 117 135

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