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• W2026360046 abstract "Lower Silurian (mid-Llandovery) carbonate rocks of the Oslo Region reflect deposition in a knoll reef platform environment. Facies patterns reflect the m migration of four laterally coexisting facies belts. Twenty microfacies types are described, most of them fitting one of the categories of the standard microfacies (SMF) concept. A shallowing and subsequent deepening phase of the depositional environment is indicated, the entire development reflecting a continuous, rather rapid relative rise of sea level." @default.
• W2026360046 created "2016-06-24" @default.
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• W2026360046 date "1987-02-01" @default.
• W2026360046 modified "2023-10-18" @default.
• W2026360046 title "A lower silurian transgressive carbonate succession in Ringerike (Oslo Region, Norway)" @default.
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• W2026360046 doi "https://doi.org/10.1016/0037-0738(87)90049-2" @default.
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