Paleomagnetism and rock magnetism of the ca. 1.87 Ga Pearson Formation, Northwest Territories, Canada: A test of vertical-axis rotation within the Great Slave basin

Paleomagnetism and rock magnetism of the ca. 1.87 Ga Pearson Formation, Northwest Territories, Canada: A test of vertical-axis rotation within the Great Slave basin

A geometrically quantitative plate-kinematic model, based on paleomagnetism, for the initial assembly of Laurentia has taken form in the past few decades. Within this framework, there remains but one problematic interval of data predominantly from the Slave craton, which is the 1.96–1.87 Ga Coronati...

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Bibliographic Details
Main Authors: Gong, Z., Xu, X., Evans, D., Hoffman, P., Mitchell, Ross, Bleeker, W.
Format: Journal Article
Published: Elsevier BV 2018
Online Access:http://hdl.handle.net/20.500.11937/67274

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