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especially for the Ordovician
The development of theories that link structure
concentrating on feedback mechanisms within ancient and evolving orogens by which individual or linked tectonic processes may influence or predetermine the operation of other processes in space and time
where Davis et al
and paleogeographic patterns correlate strongly with the dynamics of the subduction zone
The Columbia River Flood Basalt Province 1-1-001-322-4330-322 especially for the OrdovicianEditors: Stephen P. Reidel, Victor E. Camp, Martin E. Ross, John A. Wolff, Barton S. Martin, Terry L. Tolan, and Ray E. Wells Buy the e book (not available in print) The Miocene Columbia River flood basalt province covers ~210,000 km2 of the Pacific Northwest of the United States, and forms part of a larger volcanic region that also includes contemporaneous silicic centers in northern Nevada, the basaltic and time transgressive rhyolitic volcanic