Neoproterozoic–early Paleozoic provenance evolution of sedimentary rocks in and adjacent to the Farewell terrane (interior Alaska)-Reference-Cited by-同舟云学术

Neoproterozoic–early Paleozoic provenance evolution of sedimentary rocks in and adjacent to the Farewell terrane (interior Alaska)

Published:2018-02-26 Issue:2 Volume:14 Page:367-394
ISSN:1553-040X
Container-title:Geosphere
language:en
Short-container-title:

Author:

Dumoulin Julie A.¹,Jones James V.¹,Bradley Dwight C.²,Till Alison B.¹,Box Stephen E.³,O’Sullivan Paul⁴

Affiliation:

1. U.S. Geological Survey, Alaska Science Center, 4210 University Dr., Anchorage, Alaska 99508, USA

2. Retired, U.S. Geological Survey, Anchorage, Alaska 99508, USA

3. U.S. Geological Survey, Spokane, Washington 99201, USA

4. GeoSep Services, 1521 Pine Cone Road, Moscow, Idaho 83843, USA

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Link

https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/14/2/367/4101654/367.pdf

Reference81 articles.

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2. U-Pb age of detrital zircons from the Upper Precambrian terrigenous section of North Timan;Andreichev;Doklady Earth Sciences,2013

3. Late Silurian reconstruction indicated by migration of reef biota between Alaska, Baltica (Urals), and Siberia (Salair);Antoshkina;GFF,2006

4. Using fossil “fingerprints” to circumscribe the paleogeography of two Alaskan terranes along the Uralian Seaway in the Late Silurian;Antoshkina;Vestnik,2016

5. Geochemical and Nd-Sr-Pb isotopic evolution of metabasites from rifting of continental lithosphere, Seward Peninsula, Alaska, and implications for paleogeographic reconstruction;Ayuso,2014

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