Paleomagnetism of ca. 2.13–2.11 Ga Indin and ca. 1.885 Ga Ghost dyke swarms of the Slave craton: Implications for the Slave craton APW path and relative drift of Slave, Superior and Siberian cratons in the Paleoproterozoic-Reference-Cited by-同舟云学术

Paleomagnetism of ca. 2.13–2.11 Ga Indin and ca. 1.885 Ga Ghost dyke swarms of the Slave craton: Implications for the Slave craton APW path and relative drift of Slave, Superior and Siberian cratons in the Paleoproterozoic

Published:2016-04 Issue: Volume:275 Page:151-175
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Buchan Kenneth L.,Mitchell Ross N.,Bleeker Wouter,Hamilton Michael A.,LeCheminant Anthony N.

Funder

Yale University

NSF

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference131 articles.

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2. Palaeoproterozoic porphyry Cu-Au, intrusion-hosted Au and ultramafic Cu-Ni deposits in the Fennoscandian Shield: temporal constraints using U-Pb geochronology;Bejgarn;Lithos,2013

3. The Archean record: a puzzle in ca. 35 pieces;Bleeker;Lithos,2003

4. The 1991–1996 NATMAP Slave Province Project: introduction;Bleeker;Can. J. Earth Sci.,1999

5. Short-lived mantle generated magmatic events and their dyke swarms: the key to unlocking Earth's paleogeographic record back to 2. 6 Ga;Bleeker,2006

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