Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaci...
Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event
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Cairo, Egypt: Hindawi Publishing Corporation
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English
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Cairo, Egypt: Hindawi Publishing Corporation
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Geochemical conditions in intracratonic sedimentary basins are currently reducing, even at relatively shallow depths. However, during glaciation-deglaciation events, glacial meltwater production may result in enhanced recharge (Bea et al., 2011; and Bea et al., 2016) potentially having high concentrations of dissolved oxygen (O2). In this study, th...
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Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event
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TN_cdi_doaj_primary_oai_doaj_org_article_2ab5267868244dbab2532cdccf9e0394
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2ab5267868244dbab2532cdccf9e0394
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ISSN
1468-8115
E-ISSN
1468-8123
DOI
10.1155/2018/9475741
