Age and petrogenesis of the Sarmiento ophiolite complex of southern Chile

Zircon fractions separated from fine-grained plagiogranites, interpreted to be cogenetic with the mafic rocks of the Sarmiento ophiolite complex in southern Chile, yield slightly to grossly discordant age patterns for which the lower concordia intercept U-Pb ages of 140.7 +/- 0.7 Ma (Lolos Fjord) an...

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Bibliographic Details
Published in:Journal of South American Earth Sciences
Main Authors: Stern, C. R., Mukasa, Samuel B., Fuenzalida P. , R.
Other Authors: Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063, USA, Department of Geological Sciences, University of Colorado, Boulder, CO 80309-0250, USA, Empresa Nacional del Petroleo, Casilla 11135, Santiago, Chile
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 1992
Subjects:
Online Access:http://hdl.handle.net/2027.42/29957
http://www.sciencedirect.com/science/article/B6VDS-48B0P51-23/2/16d4ffe896c5a08829cd6a8953ec3e85
https://doi.org/10.1016/0895-9811(92)90020-Y