Salt dissolution tectonism and microbial origin of drainage-line silcrete in the Lower Cretaceous Athabasca Oil Sands, foreland Alberta Basin-Reference-Cited by-同舟云学术

Salt dissolution tectonism and microbial origin of drainage-line silcrete in the Lower Cretaceous Athabasca Oil Sands, foreland Alberta Basin

Published:2020-02 Issue: Volume:112 Page:104099
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Broughton Paul L.

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference117 articles.

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5. Sedimentological and stratigraphic characterization of Cretaceous upper McMurray deposits in the southern Athabasca oil sands, Alberta, Canada;Baniak;Am. Assoc. Petrol. Geol. Bull.,2018

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1. Role of co-existing ions in the removal of dissolved silica by ceramic nanofiltration membrane;Journal of Water Process Engineering;2023-07

2. Migrations of Devonian brine up-section and the origin of calcite-cemented sand in the Lower Cretaceous McMurray Formation, Athabasca Oil Sands;Canadian Journal of Earth Sciences;2022-09-01

3. Low-accommodation foreland basin response to long-term transgression: A record of change from continental-fluvial and marginal-marine to open-marine sequences over 60,000 km2 in the western Canada foreland basin;Marine and Petroleum Geology;2022-05

4. Salt dissolution tectonism and origin of lacustrine carbonate beds: Mn‐Fe‐calcite and Mn‐siderite micro‐spherulite fabrics of the Lower Cretaceous McMurray Formation, Athabasca Oil Sands deposit, western Canada;The Depositional Record;2022-03

5. A critical review of the ecological status of lakes and rivers from Canada's oil sands region;Integrated Environmental Assessment and Management;2021-10-25