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About: New Mexico aulacogen     Goto   Sponge   NotDistinct   Permalink

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The New Mexico Aulacogen is a failed rift, or failed rift arm (aulacogen), that may have formed during the Cambrian and Ordovician Periods in the area from central Colorado through southern New Mexico. Its presence is inferred from pervasive alkaline and carbonatite intrusions of this age in this area. These include the of central Colorado. A smaller alkali-carbonatite complex at returns an Ar-Ar age of 518 ± 5.7 million years. The Florida Mountains uplift took place at about this same time and may be associated with this aulacogen.