Detrital zircon U-Pb ages provide provenance and chronostratigraphic information from Eocene synorogenic deposits in northwestern Argentina

Research output: Contribution to journalArticlepeer-review

79 Scopus citations

Abstract

Paleogene elastic sedimentary rocks in the Puna plateau of northwestern Argentina contain valuable information about the timing and location of early mountain building in the central Andes. Because these rocks generally lack tuffaceous facies, only paleontological ages have been available. We present U-Pb ages from detrital zircons in the conglomeratic Eocene Geste Formation of the central Puna plateau. The zircon ages indicate that the Geste Formation was derived from nearby high-relief ranges composed of Ordovician metasedimentary rocks. A small population of ca. 37-35 Ma grains also confirms the late Eocene stratigraphic age of the Geste Formation, and suggests that U-Pb detrital zircon ages may provide a new tool for determining depositional ages and provenance of widespread Paleogene deposits in the central Andes.

Original languageEnglish (US)
Pages (from-to)323-326
Number of pages4
JournalGeology
Volume35
Issue number4
DOIs
StatePublished - Apr 1 2007

Keywords

  • Andes
  • Argentina
  • Syntectonic sedimentation
  • U-Pb geochronology

ASJC Scopus subject areas

  • Geology

Fingerprint

Dive into the research topics of 'Detrital zircon U-Pb ages provide provenance and chronostratigraphic information from Eocene synorogenic deposits in northwestern Argentina'. Together they form a unique fingerprint.

Cite this