Carboniferous quartz arenites and ganisters of the Northern Pennines
The Carboniferous succession of the Northern Pennines contains a wide variety of texturally and mineralogically mature quartz arenites. These occur interbedded with less mature sandstones, shales and limestones and are common in strata. of Brigantian to Westphalian A age. The majority of these quart...
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Durham University
1981
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.279779 |