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Geofluids
Volume 2018, Article ID 9475741, 20 pages
https://doi.org/10.1155/2018/9475741
Research Article

Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event

1CONICET-IHLLA, República de Italia 780, C.C. 47, Azul, Buenos Aires B7300, Argentina
2Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2207 Main Mall, Vancouver, BC, Canada V5T 1Z4
3Department of Civil Engineering, University of New Brunswick, P.O. Box 4400, Fredericton, NB, Canada E3B 5A3

Correspondence should be addressed to Sergio A. Bea; ra.ude.necinu.aaf@aebas

Received 24 August 2017; Revised 9 February 2018; Accepted 18 February 2018; Published 24 April 2018

Academic Editor: Tianchyi Yeh

Copyright © 2018 Sergio A. Bea et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

How to Cite this Article

Sergio A. Bea, Danyang Su, K. Ulrich Mayer, and Kerry T. B. MacQuarrie, “Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event,” Geofluids, vol. 2018, Article ID 9475741, 20 pages, 2018. https://doi.org/10.1155/2018/9475741.