Publication Date:
1944-04-01
Description:
The limestone xenoliths about to be described were collected on the eastern side of Barnavave from a disused quarry situated at the junction between the “junction hybrids” and the surrounding Carboniferous limestone. The material comes from loose blocks left over during quarrying operations. Both the hybrids and the metamorphosed limestones have been dealt with in detail elsewhere1 and will only be referred to incidentally here.
Print ISSN:
0016-7568
Electronic ISSN:
1469-5081
Topics:
Geosciences
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