Dating in the north west
Results from a third site, inland of Hightown, suggest that aeolian deposits previously mapped as part of the Shirdley Hill Sand were formed during the early to mid-Flandrian.
These aeolian sediments, which were partially buried by estuarine silts during the later Flandrian transgression, may have been derived from marine or estuarine beach deposits associated with a lower sea-level.
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Multichronometric studies of the low-temperature eclogitic Tso Morari unit (Ladakh, India) place timing constraints on the early evolution of the northwest Himalayan belt.
Several isotopic systems have been used to date the eclogitization and the exhumation of the Tso Morari unit: Lu-Hf, Sm-Nd, Rb-Sr, and Ar-Ar. 55 Ma age for the eclogitization has been obtained by Lu-Hf on garnet, omphacite, and whole rock from mafic eclogite and by Sm-Nd on garnet, glaucophane, and whole rock from high-pressure metapelites.
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Although organic deposits associated with the back-barrier sediments have been dated by radiocarbon methods, the aeolian sands have not previously been dated directly.
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