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Nd- and Pb-isotope variations in the multicyclic central caldera cluster of the San Juan volcanic field, Colorado, and implications for crustal hybridization

Journal Article · · Geology; (USA)
;  [1]
  1. Univ. of Wisconsin, Madison (USA)
The {epsilon}{sub Nd} values for six large-volume (100-3000 km{sup 3}) ash-flow tuffs and associated lavas from the multicyclic central caldera cluster of the San Juan volcanic field in south-central Colorado are between those of Proterozoic crust in the region and mantle-derived basaltic magmas, and the values generally become progressively higher in progressively younger tuffs and lavas. The increase in the {epsilon}{sub Nd} values of the tuffs, from -8.0 to -6.0 with decreasing age, can be modeled by assimilation and crystal fractionation of a mantle-derived magma, accompanied by an increase of {approx} 4 units in {epsilon}{sub Nd} values of the assimilated crust. The postulated increase in {epsilon}{sub Nd} values of the crust is envisioned to have occurred by hybridization of the crust through continued injection of mantle-derived magmas during the life of the magmatic system. Decreasing {sup 206}Pb/{sup 204}Pb ratios observed in progressively younger tuffs following the initiation of caldera-related volcanism cannot, however, be solely explained by addition of mantle-derived magmas to the crust, but are more likely to reflect the transfer of lower-crustal Pb into the upper crust as the magmatic system evolved. Input of large volumes (> 300,000 km{sup 3} in the San Juan volcanic field) of mantle-derived magma resulted in extensive hybridization of preexisting crust, suggesting that large-scale silicic volcanism involves generation of large quantities of new crust.
OSTI ID:
6313787
Journal Information:
Geology; (USA), Journal Name: Geology; (USA) Vol. 18:10; ISSN GLGYB; ISSN 0091-7613
Country of Publication:
United States
Language:
English