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- W2077481674 abstract "Abstract. - The travertine rocks building at emergences, dams and waterfalls results of biolithogenesis processes with algae and mosses supports and bacterian precipitation of Ca. Most of the deposits shows a stromatolitic laminated fades, with alternatively light and dark layers. Dark layers, which are rich in organic matter, growth in spring (Morocco) or in summer (SE of France). In «alluvial», detrital fades, bio-chemical and physical-chemical phenomena are mixed. All study of ancient deposit should claim detailed stratigraphy and micrographie determination of fades, in order to support paleogeographic interpretation tentative." @default.
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- W2077481674 date "1981-01-01" @default.
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- W2077481674 title "Thème III. Stratigraphie et pétrographie des formations travertineuses (Stratigraphy and petrography of travertine rocks)" @default.
- W2077481674 doi "https://doi.org/10.3406/bagf.1981.5255" @default.
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