Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/88995
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Type: Journal article
Title: Continental thermal isostasy: 2. Application to North America
Author: Hasterok, D.
Chapman, D.
Citation: Journal of Geophysical Research, 2007; 112(B6):B06415-1-B06415-16
Publisher: American Geophysical Union
Issue Date: 2007
ISSN: 0148-0227
2169-9356
Statement of
Responsibility: 
Derrick Hasterok, and David S. Chapman
Abstract: Continental elevations can be partitioned into contributions from thermal and compositional buoyancy and geodynamic forces. In order to isolate the thermal component, elevations of 36 North American tectonic provinces are adjusted for the effects of compositional thickness and density variations by computing an isostatic adjustment relative to a standard crustal section (2850 kg m-3 density and 39 km thickness). Crustal densities are estimated using an empirical velocity-density relationship. Compositional elevation adjustments applied to North American provinces range from ∼-1100 m in the southern Rocky Mountains to 2300 m in the Gulf of California, with uncertainties ranging from ∼200 in to >600 m. Theoretical thermal buoyancy is estimated by integrating the difference between a geotherm, derived from observed values of heat flow and a reference geotherm. The best fitting continental heat flow-elevation model has a reference heat flow of 46.6 mW m-2 at 0 km and a 60:40 partitioning of surface heat flow between reduced and upper crustal radiogenic heat flow. Raw elevations of continental provinces show little correlation with heat flow, while compositionally adjusted elevations show a clear trend with ∼3 km difference between hot and cold provinces. A continental heat flow-elevation plot is used to identify outliers in adjusted province elevations. Anomalous elevations may reflect a nonsteady state thermal regime, dynamically supported elevation, anomalous mantle, or some combination of these states. Discriminating between these elevation sources provides insight into the geodynamics of North America, demonstrating the usefulness of this approach in continental geodynamic studies. Copyright 2007 by the American Geophysical Union.
Keywords: thermal isostasy; continental elevation; North America
Rights: Copyright 2007 by the American Geophysical Union.
DOI: 10.1029/2006JB004664
Appears in Collections:Aurora harvest 7
Geology & Geophysics publications

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