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Ron Blakey

Thank you, Professor Blakey, for having served as an AAPG Distinguished Lecturer for FY 2012-13.

Ronald C. Blakey

Professor Emeritus,
Northern Arizona University; Colorado Plateau Geosystems

Funded by the AAPG Foundation

Ron Blakey is recently Professor Emeritus at Northern Arizona University following 34 years of teaching and research in the Department of Geology. During his tenure at NAU, he studied and published on the stratigraphy and sedimentology of many Late Paleozoic and Mesozoic rock units on the Colorado Plateau. His specific interests are eolian and fluvial depositional systems. This nurtured his interest in paleogeography and for the last 15 years, he has been heavily involved in producing paleogeographic maps that range from regional to global in scope. Many of these maps appear on his two websites, jan.ucc.nau.edu/~rcb7 and cpgeosystems.com. His latest endeavors have merged these two disciplines into books published by the Grand Canyon Association, "Ancient Landscapes of the Colorado Plateau" and Springer, “Plate Tectonics, Continental Drift, and Mountain Building”. His degrees are from Wisconsin (BS), Utah (MS), and Iowa (PhD).

Abstract: Using Paleogeographic Maps to Portray Phanerozoic Geologic and Paleotectonic History of Western North America

Paleogeographic maps provide clear, concise pictures of the evolving complex geologic events of Western North America. Time slices are selected to show critical stages in the geologic history thereby providing a continuous view of the evolution of the region and clearly showing sequences of paleogeography and paleotectonics. The maps are particularly effective in demonstrating the geometry and history of terrane accretion and the affects of accretionary events on the growth of Western North America from Devonian to Present. The maps are also powerful tools for comparing varying or contrasting models of various terrane-accretion events and for showing cause and effect across broad geologic provinces. Other maps (isopach, paleogeology, facies, paleocurrent, etc.) can be used in conjunction with paleogeographic maps to further explain the geologic history.

The models presented here are derived and modified from the geologic literature. Data is plotted on basemaps and paleogeography is cloned from digital elevation maps to match the inferred distribution of landforms at given times and places. The paleogeography is shown in palinspastic restoration with reference to present political boundaries. The maps are finished in a fashion to show how paleogeography might have appeared as if seen from space. Colors suggest paleovegetation and inferred paleoclimate. Water depths are shown in shades of blue from evidence presented in the literature and presumed modern analogs. Although maps are assigned a specific geologic age, ranges are given to suggest the interval for which the maps are valid. The resulting series of paleogeographic maps provides a coherent picture of the geologic and tectonic history of Western North America that respects known and inferred geologic rates and geodynamic models.

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