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- W2883249533 abstract "The clay mineralogy of Mid-Cretaceous carbonate pelagic sediments of the Maiella Mountain, a transition zone between the Abruzzi platform and the Umbrian basin, have been studied by X-ray diffraction and transmission electron microscopy. The clay assemblages are composed of chlorite, illite, smectite, illite/smectite mixed-layers and detrital palygorskite. The palygorskite occurs only in sediments deposited during anoxic periods. These periods are associated with sea-level rises, and therefore it is suggested that during Mid-Cretaceous, in the basin of the Maiella Mountain, palygorskite was derived from the reworking of pedogenic crusts or chemical sediments which were deposited on the adjacent platform areas during transgressive events." @default.
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- W2883249533 date "1990-01-01" @default.
- W2883249533 modified "2023-10-18" @default.
- W2883249533 title "Palygorskite and eustatism during Mid-Cretaceous in the Maiella Mountain (Abruzzi, Central Italy)" @default.
- W2883249533 hasPublicationYear "1990" @default.
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