Abstract
New K-Ar and Rb-Sr data have been obtained for Precambrian rocks of north-central New Mexico. K-Ar dates fall into one group with a mean of 1,325 ± 13 m.y. and another with a mean of 1,257 ± 21 m.y. The former conforms to the 1,350-m.y. B.P. event reported in previous literature. The latter defines a 1,250-m.y. B.P. event that is both tectonic and hydrothermal. Limited new Rb-Sr data support a 1,425-m.y. isochron. Thus, there are four events for the Precambrian rocks of northern New Mexico: (1) 1,673-m.y. B.P. intrusion of “Embudo Granite”; (2) 1,425-m.y. B.P. tectonic and metamorphic event accompanied by pegmatite emplacement; (3) 1,350-m.y. B.P. thermal event; and (4) 1,250-m.y. B.P. tectonic and hydrothermal event.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.