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This conversation with Hilary Corlett is about understanding dolomite diagenesis by analyzing elements and isotopes in age equivalent calcite and dolomite filled burrows. It is based on Hilary Corlett and Brian Jones's\\xa0 technical article titled \\u201cPetrographic and Geochemical Contrasts Between Calcite and Dolomite Filled Burrows in the Middle Devonian Lonely Bay Formation, Northwest Territories, Canada: Implications for Dolomite Formation in Paleozoic Burrows\\u201d. \\xa0
What is the importance of bioturbation in dolomitization?\\xa0 What geochemical differences are seen between calcite fills and dolomite fills?\\xa0 What does a diagenetic halo look like?\\xa0 Which borrow fill is more proximal?\\xa0 Which burrow type represents anoxic deposition?\\xa0 \\xa0
May this exchange serve to expand your geological knowledge on the go.
For more information go to www.stoneconsulting.info
Citation: Hilary J. Corlett, Brian Jones; Petrographic and Geochemical Contrasts Between Calcite- and Dolomite-Filled Burrows In the Middle Devonian Lonely Bay Formation, Northwest Territories, Canada: Implications for Dolomite Formation In Paleozoic Burrows. Journal of Sedimentary Research ; 82 (9): 648\\u2013663.\\xa0
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