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Uranium-lead geochronology of the Archean Imataca Series, Venezuelan Guayana Shield

✍ Scribed by Carla W. Montgomery


Publisher
Springer
Year
1979
Tongue
English
Weight
910 KB
Volume
69
Category
Article
ISSN
0010-7999

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✦ Synopsis


Uranium and lead isotopic analyses of totalrock and feldspar samples from the Imataca Series indicate an early Archean (3.5 + b,y.) age for the basement gneisses. Lead isotopic evolution in most gneiss samples may approximately be described by a three-stage model. The start of the third stage is marked by a pervasive metamorphic event, locally up to pyroxene-granulite grade, at 2 b.y. ago, which commonly resulted in extensive depletion of uranium relative to lead.