2021
DOI: 10.1016/j.marpetgeo.2021.105066
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Compositional and diagenetic evolution of a siltstone, with implications for reservoir quality; an example from the Lower Triassic Montney Formation in western Canada

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Cited by 11 publications
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“…Because of these reasons, the deposited sediment predominantly consisted of quartz, chert, feldspars, dolomite, and mixed-layer I/S clays. For a long time, scientists disagreed on whether or not the Montney Formation contained any clay minerals in appreciable amounts [23]. Authigenic clay precipitation occurred in an intermediate stage, followed by quartz and feldspar dissolution and the second phase of carbonate precipitation [24].…”
Section: Geological Backgroundmentioning
confidence: 99%
“…Because of these reasons, the deposited sediment predominantly consisted of quartz, chert, feldspars, dolomite, and mixed-layer I/S clays. For a long time, scientists disagreed on whether or not the Montney Formation contained any clay minerals in appreciable amounts [23]. Authigenic clay precipitation occurred in an intermediate stage, followed by quartz and feldspar dissolution and the second phase of carbonate precipitation [24].…”
Section: Geological Backgroundmentioning
confidence: 99%