Stromatolites and fenestral fabric in Early Proterozoic Huronian Supergroup, Ontario
- 1 October 1980
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 17 (10) , 1351-1357
- https://doi.org/10.1139/e80-142
Abstract
Crustose and columnar carbonate stromatolites from the Espanola Formation at Quirke Lake, and laminated dolostone with fenestral fabric from the Gordon Lake Formation at Plummer, are considered to be products of benthic microbial activity at isolated, carbonate accumulating sites in transitional environments characterized almost exclusively by arenaceous sedimentation.This publication has 0 references indexed in Scilit: