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- W1998267918 abstract "SUMMARY The Lower and Upper Haslingden Flags may be differentiated from other Yeadonian strata in the Pennine Basin by their bulk lithology (‘green-facies’) and the reworked palynomorphs that they contain. These characteristics allow correlative finer-grained sedimentary rocks to be recognized where arenaceous lithologies have died out, and put some constraints on the possible provenance of the Haslingden Flags. The source area must have included outcrops of unmetamorphosed (i.e. extra-Caledonide) Lower Palaeozoic rocks and marine Devonian strata, and/or marine Devonian sediments containing reworked Lower Palaeozoic palynomorphs. Previous palaeocurrent studies indicate a western provenance for the Haslingden Flags. The new palynological data suggest that some sediment may have come directly from Avalonian Ordovician terranes: suitable source areas extend from the Wales-Brabant High (St George’s Land) towards Newfoundland. However, the reworked palynomorph material may have been supplied to the Pennine Basin via multiple phases of reworking, involving marine Devonian rocks to the west of St George’s Land." @default.
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- W1998267918 date "1996-11-01" @default.
- W1998267918 modified "2023-09-23" @default.
- W1998267918 title "Reworked palynomorphs as provenance indicators in the Yeadonian of the Pennine Basin" @default.
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- W1998267918 doi "https://doi.org/10.1144/pygs.51.2.141" @default.
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