2011年
A procedure for calculating a consistent set of closure temperatures and cooling rate using Dodson’s formula
Journal of Geological Society of Japan
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- 巻
- 117
- 号
- 2
- 開始ページ
- 99
- 終了ページ
- 103
- 記述言語
- 英語
- 掲載種別
- 研究論文(学術雑誌)
- DOI
- 10.5575/geosoc.117.99
- 出版者・発行元
- The Geological Society of Japan
The cooling rate of a geological material is generally calculated using two isotopic ages with different closure temperatures; however, the closure temperature is itself dependent on the cooling rate. Here we present a simple procedure for calculating a consistent set of closure temperatures and cooling rate using Dodson's mathematical formula.
- リンク情報
- ID情報
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- DOI : 10.5575/geosoc.117.99
- ISSN : 0016-7630
- ISSN : 1349-9963
- CiNii Articles ID : 130000758388
- CiNii Books ID : AN00141768