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- W2085479920 abstract "A Mesozoic continental margin sequence in the Othris Mountains, eastern Greece, contains a variety of both primary and replacement cherts occurring in several stratigraphic positions. Primary cherts, defined as these derived from siliceous sediment, show differences in bedform, sedimentary structures, mineralogy and chemistry. Examples described illustrate deposition by turbidity currents, traction currents and an in-situ pelagic “rain”. Chemical analyses show that major elements can be used to discriminate between different chert formations. Iron and manganese enrichment is a feature of cherts which have been deposited under steady sedimentation conditions. Stratigraphic relationships prove the older, current-deposited, Othris cherts to have been deposites on a volcanic ocean ridge where they probably accumulated in topographic depressions, and also between the ridge and the lower continental margin where they were deposited mainly by turbidites derived from an oceanic source. A younger suite which covers calcareous shelf, marginal and pelagic sediments is an in-situ deposit. These inferences illustrate how primary cherts can add to interpretations of ancient oceanic terrains by providing information on sea-floor topography and, potentially, circulation patterns. Some cherts can be used as facing indicators in sequences where no other wayup evidence is available." @default.
- W2085479920 created "2016-06-24" @default.
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- W2085479920 date "1977-08-01" @default.
- W2085479920 modified "2023-09-25" @default.
- W2085479920 title "Facies distinction and interpretation of primary cherts in a mesozoic continental margin succession, Othris, Greece" @default.
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- W2085479920 doi "https://doi.org/10.1016/0037-0738(77)90057-4" @default.
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