A procedure for calculating a consistent set of closure temperatures and cooling rate using Dodson’s formula
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概要
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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.
著者
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Itaya Tetsumaru
Research Institute Of National Sciences Okayama University Of Science
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MAEDA Jinichiro
Department of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University
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Zeniya Ryoichi
Department Of Earth And Planetary Sciences Graduate School Of Science Hokkaido University
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Kuramoto Yoshiyuki
Department of Natural History Sciences, Faculty of Science, Hokkaido University
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Kagami Hiroo
2053-16,
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Itaya Tetsumaru
Research Insitute of Natural Science,Okayama University of Science
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Kagami Hiroo
2053-16, <span style="text-decoration:overline;">O</span>machi, <span style="text-decoration:overline;">O</span>machi, Nagano 398-0002, Japan
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Zeniya Ryoichi
Department of Natural History Sciences, Faculty of Science, Hokkaido University
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