dc.description.abstract | The hebridean area is well known for the spectacular
Palaeocene igneous rocks (plutons, dykes, sills and
flood basalts) that form part of the North Atlantic
large igneous province. The exposures of Mesozoic
sedimentary strata of the Hebrides have been less
widely appreciated, partly because they are
perceived as having been extensively altered by
thermal metamorphism. Whilst this is undoubtedly
true locally, the bulk of the succession remains only
weakly affected, and much of significance has been
learned from it of Jurassic palaeoenvironments,
biostratigraphy and magnetostratigraphy.
Additionally, because of recent hydrocarbon
exploration in the Mesozoic basins offshore west of
Scotland and Ireland (Trueblood & Morton, 1991;
Fyfe et al., 1993; Stoker et al., 1993; Scotchman &
Thomas, 1995) these succession have assumed a
new importance as the nearest easily accessible
outcrop analogues | en_GB |