NEOPROTEROZOIC-PALEOZOIC TECTONICS AND PALEOGEOGRAPHY OF THE WEST-CENTRAL SOUTH AMERICA CONVERGENT MARGIN FROM DETRITAL ZIRCON GEOCHRONOLOGY

2017 ◽  
Author(s):  
Amanda Z. Calle ◽  
◽  
Brian K. Horton ◽  
Raúl García-Duarte ◽  
Peter P. Flaig
Keyword(s):  
South America ◽  
Detrital Zircon ◽  
Zircon Geochronology ◽  
Convergent Margin ◽  
The West ◽  
Detrital Zircon Geochronology ◽  
West Central ◽  
Central South

Detrital Zircon Geochronology of Mesozoic Sediments in the Rif and Middle Atlas Belts of Morocco: Provenance Constraints and Refinement of the West African Signature

2015 ◽  
Vol 123 (2) ◽  
pp. 177-200 ◽  
Author(s):  
Jonathan R. Pratt ◽  
David L. Barbeau ◽  
John I. Garver ◽  
Anas Emran ◽  
Tyler M. Izykowski
Keyword(s):  
Detrital Zircon ◽  
West African ◽  
Zircon Geochronology ◽  
The West ◽  
Detrital Zircon Geochronology ◽  
Middle Atlas

scholarly journals Detrital Zircon Geochronology of Cretaceous and Paleogene Strata Across the South-Central Alaskan Convergent Margin

2009 ◽  
Author(s):  
Dwight Bradley ◽  
Peter J. Haeussler ◽  
Paul O'Sullivan ◽  
Rich Friedman ◽  
Alison Till ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Zircon Geochronology ◽  
The South ◽  
Convergent Margin ◽  
Detrital Zircon Geochronology ◽  
South Central

Detrital zircon geochronology of the Taku terrane, southeast Alaska

2002 ◽  
Vol 39 (6) ◽  
pp. 921-931 ◽  
Author(s):  
George E Gehrels
Keyword(s):  
Detrital Zircon ◽  
Detrital Zircons ◽  
Zircon Geochronology ◽  
The West ◽  
Southeast Alaska ◽  
Detrital Zircon Geochronology ◽  
Tectonic Boundary ◽  
Alexander Terrane

U–Pb geochronologic studies have been conducted on 60 detrital zircon grains from Permian(?) and Triassic metasandstones of the Taku terrane in central southeast Alaska. The resulting ages are mainly in the range 349–387 Ma, with five additional grains that yield probable ages ranging from ~906 to ~2643 Ma. These ages are similar to the ages of detrital zircons in Carboniferous and older rocks of the Yukon–Tanana terrane, which lies directly east of the Taku terrane. In contrast, these ages are different from the ages of detrital zircon grains in the Alexander terrane to the west. The data are accordingly consistent with models in which the Taku terrane is a western component of the Stikine and Yukon–Tanana terranes, and that this crustal fragment is separated by a fundamental tectonic boundary from rocks of the Alexander and Wrangellia terranes to the west.

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