Palaeomagnetism and magnetic–polarity zonation in some Oligocene volcanic rocks of the San Juan Mountains, south–western Colorado

Geophysical Journal International
By: , and 

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Abstract

Palaeomagnetic results have been obtained from thirty sites in intrusive and extrusive rocks of Oligocene age from the San Juan Mountains, south-western Colorado. All specimens from each site were subjected to af demagnetization, and the reliability of each site determined. Twenty-three sites gave reliable results. Because five sites from the thick intracaldera part of the La Jara Canyon Member of the Treasure Mountain Tuff appear to have become magnetized during the same small interval of geological time, their results were combined and their mean pole and direction used in the final calculations. The eighteen remaining reliable sites yielded an average Oligocene palaeomagnetic pole at 85·6° N and 298·0° E (δp = 8°, δm = 11°, k = 24·1). A stratigraphic sequence is given for the major San Juan ash-flow sheets and selected additional units with their corresponding magnetic polarities and mean K-Ar ages.

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Publication type Article
Publication Subtype Journal Article
Title Palaeomagnetism and magnetic–polarity zonation in some Oligocene volcanic rocks of the San Juan Mountains, south–western Colorado
Series title Geophysical Journal International
DOI 10.1111/j.1365-246X.1974.tb01242.x
Volume 37
Issue 2
Year Published 1974
Language English
Publisher Oxford Academic
Contributing office(s) Volcano Science Center
Description 10 p.
First page 323
Last page 332
Country United States
State Colorado
Other Geospatial San Juan Mountains
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