Late Jurassic palaeoclimatic change from clay mineralogy and gamma-ray spectrometry of the Kimmeridge Clay, Dorset, UK

The Late Jurassic was a time of increasing aridity in NW Europe. Here, a new clay mineral dataset is presented from a 600 m thick composite core through the Kimmeridge Clay Formation, southern England. Clay mineral assemblages comprise mainly illite and kaolinite, with minor randomly interstratified...

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מידע ביבליוגרפי
Main Authors: Hesselbo, S, Deconinck, J, Huggett, J, Morgans-Bell, H
פורמט: Journal article
שפה:English
יצא לאור: 2009

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