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The Culpeper basin is a north-northeast-trending faulted trough at the inner margin of the Piedmont geologic province along the east front of the Blue Ridge. Most of the Culpeper Group is intruded and locally metamorphosed by dikes, sills, and stocks of tholeiitic diabase. This report deals with a suite of samples from several diabase intrusives and basalt flows in the northern part of the Culpeper basin in Virginia. 22 refs., 2 figs., 2 tabs. (ACR)

Geochemical data for Jurassic diabase and basalt of the northern Culpeper basin, Virginia