Provenance and tectonic implications of Orán Group foreland basin sediments, Río Iruya canyon, NW Argentina (23° S)
Author:
Affiliation:
1. Middlebury College Geology Department Middlebury VTUSA
2. Earth Research Institute University of California Santa Barbara CAUSA
3. Departamento de Geología Universidad Nacional de Salta Salta Argentina
Funder
National Science Foundation
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12139
Reference75 articles.
1. Trace elements in quartz shed light on sediment provenance
2. The Pacific Gondwana margin in the late Neoproterozoic–early Paleozoic: Detrital zircon U–Pb ages from metasediments in northwest Argentina reveal their maximum age, provenance and tectonic setting
3. THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES
4. Construction of detrital mineral populations: insights from mixing of U-Pb zircon ages in Himalayan rivers
5. U–Pb zircon ages as a sediment mixing tracer in the Nepal Himalaya
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