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• W2012310214 abstract "The Kastellios Hill section is situated in central Crete and composed mainly of mudstones and silts deposited in lacustrine, brackish or estuarine environments. Several levels of this section have yielded the remains of mammals, foraminifera, ostracoda, pollen and spores. The palynological analysis shows that the region was forested in the Upper Miocene, with a vegetation confined to climates warmer than the present. The age indicated by foraminifera is Early Tortonian, while the mammals were attributed to Late Vallesian in continental biochronology. Of this section 88 m have been sampled for a magnetostratigraphic study. Several experiments have been made on the magnetic properties of these sediments showing that they are suitable for a paleomagnetic study. Moreover, X-ray diffraction and microprobe analysis of 19 samples regularly distributed over the section show that no major changes occurred in the chemical composition. From 77 separate sites, 241 samples have been demagnetized, thermally (215) or by alternating field (26). The main result of this study is the definition of a long reversed polarity period interrupted by two short normal intervals. This magnetostratigraphic sequence can be correlated, using biostratigraphic data, with a part of Chron 5 r of the geomagnetic time scale; in other words, this section is probably younger than 11.47 My and older than 10.30 My." @default.
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• W2012310214 date "1986-03-01" @default.
• W2012310214 modified "2023-10-16" @default.
• W2012310214 title "Magnetostratigraphy and biostratigraphy of the neogene deposits of Kastellios Hill (Central Crete, Greece)" @default.
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• W2012310214 doi "https://doi.org/10.1016/0031-0182(86)90066-0" @default.
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