Results 61 to 70 of about 30,510 (167)

Topographic Development History of the Alaska Range [PDF]

open access: yes, 2013
he overall goal of this project is to use variations in sediment source through time as a proxy for deciphering the uplift history of the Alaska Range (Fig. 1).
Davis, Kailyn
core  

U-Pb zircon ages of Early Archean gneisses from northern Labrador

open access: yesU-Pb zircon ages of Early Archean gneisses from northern Labrador
Early Archean crustal records are rare, but contiguous units are best preserved in N. Labrador and the NWT (Canada) and in SW Greenland. The Saglek-Hebron area (N. Labrador), located at the W. extension of the North Atlantic Craton (NAC), contains wellpreserved Eo-Paleoarchean suites including pre-3.8 Ga Nanok Ferich monzodioritic gneiss, the Nulliak ...
openaire   +1 more source

Shrimp U-Pb Ages of Detrital Zircons in Sargurs

open access: yesJournal Geological Society of India, 1993
A. P. Nutman   +3 more
openaire   +1 more source

Zircon U-Pb age data, Ray Mountains area, Bettles Quadrangle, Alaska [PDF]

open access: yes, 2016
A. L. Tuzzolino   +3 more
openaire   +1 more source

Contemporaneous mobile- and stagnant-lid tectonics on the Hadean Earth. [PDF]

open access: yesNature
Valley JW   +11 more
europepmc   +1 more source

Tectonism rather than "snowball Earth" glaciation is responsible for the Great Unconformity. [PDF]

open access: yesProc Natl Acad Sci U S A
Zhan RR   +11 more
europepmc   +1 more source

Ion microprobe zircon geochronology of the Uivak Gneisses: Implications for the evolution of early terrestrial crust in the North Atlantic Craton [PDF]

open access: yes
Ion microprobe U-Pb results for zircons from three Uivak I gneisses and one specimen of Uivak II gneiss, from the Saglek-Hebron area of Northern Labrador are reported.
Collerson, K. D.
core   +1 more source

Reconstructing Eocene Antarctic river drainage from provenance analysis of Amundsen Sea embayment sediments. [PDF]

open access: yesSci Adv
Marschalek JW   +15 more
europepmc   +1 more source

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