Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5780478 | Journal of South American Earth Sciences | 2017 | 59 Pages |
Abstract
U-Pb data of zircons indicated two age populations, with predominance of Permian-Triassic (â¼216-286 Ma) and Neoproterozoic (â¼551-996 Ma). The Permian-Triassic zircons were contributed by the granitoids and recycled metasedimentary rocks of the Chiapas Massif Complex. The major contribution of Neoproterozoic zircons was from the Chaucus, Oaxacan, and Chiapas Massif Complexes in Grenville Province, southern Mexico. U-Pb ages of zircons from the Brujas beach are consistent to the reported zircon ages from the drainage basins of Usumacinta, Coatzacoalcos, and Grijalva Rivers in southern Mexico, suggesting that the sediments delivered by the rivers to the beach area are vital in defining the provenance of placers.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Hector J. Tapia-Fernandez, John S. Armstrong-Altrin, Kandasamy Selvaraj,