Printer Friendly

Groundwater silcrete in the Potsdam Group, Ottawa Graben, Canada: a case example of shallow fault-controlled silicification and desilicification in a tectonically active basin.

Silcrete forms by silicification of sediment or bedrock at the Earth's surface due to soil-forming processes (pedogenic silcrete), or in the shallow subsurface (< 100 m) along the water table (groundwater silcrete). Unlike pedogenic silcretes, the origin of groundwater silcretes are poorly understood with existing case studies highlighting near-surface silica flux, whereas extrabasinal sources and/or migration of silica-bearing fluids along faults have not been demonstrated. Based on spatial and textural characteristics of a groundwater silcrete from the Cambrian-Ordovician Potsdam Group in the Ottawa Graben, however, a close association between the migration of silica-rich fluids and multiple northeast-trending faults is suggested. This [less than or equal to]150 cm-thick silcrete horizon underlies an unconformity that caps a succession of fluvial quartz arenite along the flanks of fault-bounded ridges of Grenville basement. The silcrete horizon thickens toward these faults and shows a systematic change in morphology from nodular to massive to brecciated. Cathodoluminescence reveals an early luminescent zoned cement (C1) associated with silcrete formation, and a later massive non-luminescent cement (C2) that occurs as overgrows filling remaining porosity in these and adjacent Potsdam strata. Fracturing and autoclastic brecciation of silcrete occurs within tens of meters of faults and is characterized by jigsaw and collapse breccia made up of silcrete clasts in a massive sand, kaolinite, and Feoxide matrix. Here it is speculated that silica-rich fluids moved along faults and advected into adjacent Potsdam sediment where the effects of pH change and evaporation promoted C1 precipitation. Later fracturing and migration of high pH fluids near faults led to local Cl dissolution and autoclastic brecciation. Finally, C2 cements formed throughout Potsdam strata following burial and pressure solution of non-silcretized arenite. Although the source of silica and fluid reservoirs for Cl remains uncertain, the scarcity of remnant detrital feldspar or unstable silicates in Potsdam strata suggests that the Grenville basement was the most likely source. Ongoing fluid inclusion analyses of Cl cements aims to resolve fluid temperature and salinity conditions, and a meteoric versus hydrothermal origin.

DAVID LOWE (1), RWC ARNOTT (2), EDWARD DESANTIS (3), AND JAMES CONLIFFE (4)

1. Department of Earth Sciences, Memorial University, St. John's, Newfoundland and Labrador A1B 3X5, Canada <dlowe@mun.ca>;

2. Department of Earth and Environmental Sciences, Ottawa University, Ottawa, Ontario K1N 6N5, Canada;

3. Fisheries and Oceans Canada, Ottawa, Ontario K1A 0E6, Canada;

4. Geologic Survey Division, Newfoundland and Labrador Department of Industry, Energy and Technology, St. John's, Newfoundland and Labrador A1B 4J6, Canada

COPYRIGHT 2021 Atlantic Geoscience Society
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 2021 Gale, Cengage Learning. All rights reserved.

Article Details
Printer friendly Cite/link Email Feedback
Author:Lowe, David; Arnott, Rwc; Desantis, Edward; Conliffe, James
Publication:Atlantic Geology
Geographic Code:1CANA
Date:Jan 1, 2021
Words:406
Previous Article:A tale of two ponds.
Next Article:Student acceptance of digital specimens as a substitute for the real thing in an introductory geology lab.
Topics:

Terms of use | Privacy policy | Copyright © 2021 Farlex, Inc. | Feedback | For webmasters |