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- W2273359155 abstract "ABSTRACT A bed of megabreccia at the base of the Mount Hawk Formation at Mount Haultain, Jasper National Park, was mapped in detail along 780 ft of its length. It consists of disoriented blocks up to 125 ft across derived from the margin of the Ancient Wall carbonate bank, and can be followed for about 5000 ft from the bank margin into the argillaceous limestones of the basin facies. Stromatoporoids, corals, algae, foraminifera and bivalves in the blocks and matrix came from various facies of the bank margin. The blocks were grouped into stromatoporoid-algal, Stachyodes, skeletal calcarenite, pelmicrite, and nonskeletal calcarenite microfacies on the basis of cluster analysis. The rocks of these microfacies were probably derived from marginal bioherms and biostromes, upper bank slope and backreef environments of the carbonate complex. The blocks in the breccia broke from the unstable margin of the complex and moved down the low (10 degrees or less) slope. The movement of the larger blocks was aided by a lubricating film of mud underneath them; the smaller blocks were transported in a carbonate mud-and-fragment suspension." @default.
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- W2273359155 date "1972-09-01" @default.
- W2273359155 modified "2023-09-24" @default.
- W2273359155 title "A Devonian Megabreccia at The Margin of The Ancient Wall Carbonate Complex, Alberta" @default.
- W2273359155 doi "https://doi.org/10.35767/gscpgbull.20.3.412" @default.
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