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- W2003758314 abstract "Abstract Sedimentological, mineralogical and geochemical studies were carried out on pelitic fractions of an Apenninic deep-sea turbidite sequence (the Helmintoid Flysch Group) in order to evaluate compositional signals correlated to distinct depositional mechanisms (i.e. sedimentation vs. resedimentation) for deep-sea sediments. The studied sequence (the Solignano flysch, lower Maastrichtian) consists of resedimented siliciclastic, carbonate and composite sediments alternating with thin (few centimetres thick) beds of hemipelagic sediments low in carbonates. All of the sediments were deposited below the calcite compensation depth. X-ray diffraction, thermal (TG, DTG and DTA) and chemical analyses (major and trace elements, carbon and oxygen isotope analyses) were performed on the fine-grained fractions (" @default.
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- W2003758314 date "1998-01-01" @default.
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- W2003758314 title "Mineralogical and geochemical criteria for distinguishing turbidite and hemipelagic pelites — the Maastrichtian of the northern Apennines, Italy" @default.
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- W2003758314 doi "https://doi.org/10.1016/s0037-0738(97)00098-5" @default.
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