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Azmy, Karem.
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Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian...
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Carbon-isotope stratigraphy of the SPICE event (Upper Cambrian) in eastern Laure...
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Carbon-isotope stratigraphy of the uppermost Cambrian in eastern Laurentia: impl...
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Expanded marine anoxia at the Cambrian-Ordovician transition: Evidence from lime...
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High-resolution isotope stratigraphy of the Lower Ordovician St. George Group of...
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Dolomitization of the lower St. George Group on the Northern Peninsula in wester...
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Carbonate cementation in the Tithonian Jeanne d’Arc sandstone, Terra Nova Field,...
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High-resolution isotope stratigraphy of the Lower Ordovician St. George Group of...
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Variability of sedimentary pyrite δ34S records: A case study of slope shale of t...
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Palaeoenvironmental changes in slope carbonates across the Late Cambrian–Early O...
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In situ geochemical characterization of pyrite crystals in burial dolomites of S...
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Diagenesis and Evolution of Microporosity of Middle–Upper Devonian Kee Scarp Ree...
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In situ geochemical characterization of pyrite crystals in burial dolomites of S...
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In situ characterization of dolomite crystals: Evaluation of dolomitization proc...
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Geochemistry and diagenetic history of the Ordovician Lower Head Formation Sands...
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Geochemistry and diagenetic history of the Ordovician Lower Head Formation Sands...
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Geochemistry and diagenetic history of the Ordovician Lower Head Formation Sands...
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Geochemistry and diagenetic history of the Ordovician Lower Head Formation Sands...
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Geochemistry and diagenetic history of the Ordovician Lower Head Formation Sands...
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Geochemistry and diagenetic history of the Ordovician Lower Head Formation Sands...
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Geology
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General Earth and Planetary Sciences
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[SDE.BE]Environmental Sciences/Biodiversity and Ecology
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
acid fractionation
boat harbor formation
body temperatures
c-13-o-18 bonds
canada implications
carbonate minerals
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Brachiopod calcite
Brachiopoda
Controlled culturing experiements
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Paleo-proxy
Paleontology
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