Mineral magnetic analyses as a means of lithostratigraphic correlation and provenance indication of glacial diamicts: Intra‐ and interunit variation

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Abstract
Mineral magnetic analyses are applied to a series of diamict samples taken from the Quaternary sequence in the Isle of Man in order to assess the relative magnitude of the intra‐and inter‐unit variation of the magnetic properties. The results are analysed both qualitatively and quantitatively and show that the level of intra‐unit variation is significantly less than the level of inter‐unit variation. The intra‐unit variation detected appears to show some relationship to the basic stratigraphy. Previous correlations based upon field evidence of diamict units exposed upon the east and west coasts of the Isle of Man are supported by their mineral magnetic properties. The statistically significant differences in the magnetic mineralogy of the stratigraphically lower Wyllin and Shellag Tills and the upper Orrisdale, Ballavarkish and Ballaquark Tills suggests distinct provenances for these two suites of sediments, allowing potential source areas to be suggested. These source areas are consistent with published data on ice flow directions in the Irish Sea Basin during the Devensian.