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Quantitative examination of the cause of the Paleocene-Eocene thermal maximum using an atmosphere-ocean box model

  • Yasukawa K
  • Kato Y
The Journal of the Geological Society of Japan (2011) 117(4) 217-237
DOI: 10.5575/geosoc.117.217
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Yasukawa, K., & Kato, Y. (2011). Quantitative examination of the cause of the Paleocene-Eocene thermal maximum using an atmosphere-ocean box model. The Journal of the Geological Society of Japan, 117(4), 217–237. https://doi.org/10.5575/geosoc.117.217

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