scholarly journals Detrital-zircon geochronology of the Sawtooth metamorphic complex, Idaho: Evidence for metamorphosed lower Paleozoic shelf strata within the Idaho batholith

Geosphere ◽  
2016 ◽  
Vol 12 (4) ◽  
pp. 1136-1153 ◽  
Author(s):  
Chong Ma ◽  
Philip Bergeron ◽  
David A. Foster ◽  
Barbara L. Dutrow ◽  
Paul A. Mueller ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Zircon Geochronology ◽  
Metamorphic Complex ◽  
Lower Paleozoic ◽  
Detrital Zircon Geochronology

Detrital-zircon geochronology and provenance of the El Oro Metamorphic Complex, Ecuador: Geodynamic implications for the evolution of the western Gondwana margin

2019 ◽  
Vol 90 ◽  
pp. 520-539
Author(s):  
Nils Suhr ◽  
Yamirka Rojas-Agramonte ◽  
David M. Chew ◽  
André J. Pinto ◽  
Diego Villagómez-Díaz ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Zircon Geochronology ◽  
Metamorphic Complex ◽  
Detrital Zircon Geochronology ◽  
Gondwana Margin

Detrital zircon geochronology of Upper Proterozoic to lower Paleozoic continental margin strata of the Kootenay Arc: implications for the early Paleozoic tectonic development of the eastern Canadian Cordillera

1991 ◽  
Vol 28 (8) ◽  
pp. 1271-1284 ◽  
Author(s):  
Moira T. Smith ◽  
George E. Gehrels
Keyword(s):  
Detrital Zircon ◽  
Canadian Cordillera ◽  
Zircon Geochronology ◽  
Early Paleozoic ◽  
Lower Paleozoic ◽  
Detrital Zircon Geochronology ◽  
Upper Proterozoic ◽  
Southern Alberta ◽  
Tectonic Development

The Kootenay Arc in northeastern Washington and southeastern British Columbia contains the transition between autochthonous Upper Proterozoic to lower Paleozoic miogeoclinal strata and outboard Paleozoic to Mesozoic eugeoclinal terranes of uncertain paleogeographic affinity. To better understand the nature of this transition, U–Pb detrital zircon geochronologic studies were carried out on Upper Proterozic and lower Paleozoic sedimentary units in the Kootenay Arc, including miogeoclinal strata of the Horsethief Creek and Hamill groups and eugeoclinal strata of the Broadview and Ajax formations (Lardeau Group) and Daisy Formation (Covada Group). The results indicate that all units sampled are derived from source terranes of ~1.7 to 2.7 Ga, with notable populations of 1.76–1.85, 1.9–2.1, and 2.5–2.7 Ga zircons. These results are consistent with derivation of both the miogeoclinal and lower Paleozoic eugeoclinal units from adjacent portions of the southern Alberta craton. This extends the western limit of supracrustal rocks of known North American affinity, formed approximately in situ in the southern Canadian Cordillera, to outboard of the lower Paleozoic eugeoclinal strata in the Kootenay Arc.

FROM ISOTOPES TO ICE: CONSTRAINING SW GONDWANA ICE SOURCES VIA DETRITAL ZIRCON GEOCHRONOLOGY DURING THE LPIA

2016 ◽  
Author(s):  
Neil Griffis ◽  
◽  
Nicholas D. Fedorchuk ◽  
Isabel P. Montañez ◽  
John L. Isbell ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Zircon Geochronology ◽  
Detrital Zircon Geochronology ◽  
Sw Gondwana
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