An evaluation of Mesozoic rift-related magmatism on the margins of the Labrador Sea : implications for rifting and passive margin asymmetry.

Journal article


Phethean, Jordan, Peace, Alexander, McCaffrey, Ken, Imber, Jonathan, Nowell, Geoff, Gerdes, Keith and Dempsey, Edward 2016. An evaluation of Mesozoic rift-related magmatism on the margins of the Labrador Sea : implications for rifting and passive margin asymmetry. Geosphere. https://doi.org/10.1130/GES01341.1
AuthorsPhethean, Jordan, Peace, Alexander, McCaffrey, Ken, Imber, Jonathan, Nowell, Geoff, Gerdes, Keith and Dempsey, Edward
Abstract

The Labrador Sea is a small (~900 km wide) ocean basin separating southwest Greenland from Labrador, Canada. It opened following a series of rifting events that began as
arly as the Late Triassic or Jurassic, culminating in a brief period of seafloor spreading commencing by polarity chron 27 (C27; Danian) and ending by C13 (Eocene-Oligocene
oundary). Rift-related magmatism has been documented on both conjugate margins of the Labrador Sea. In southwest Greenland this magmatism formed a major coast-parallel dike swarm as well as other smaller dikes and intrusions. Evidence for rift-related magmatism on the conjugate Labrador margin is limited to igneous lithologies found in deep offshore exploration wells, mostly belonging to the Alexis Formation, along with a postulated Early Cretaceous nephelinite dike swarm (ca. 142 Ma) that crops out onshore, near Makkovik, Labrador. Our field observations of this Early Cretaceous nephelinite suite lead us to conclude that the early rift-related magmatism exposed around Makkovik is volumetrically and spatially limited compared to the contemporaneous magmatism on the conjugate southwest Greenland margin. This asymmetry in the spatial extent of the exposed onshore magmatism is consistent with other observations of asymmetry between the conjugate margins of the Labrador Sea, including the total sediment thickness in offshore basins, the crustal structure, and the bathymetric profile of the shelf width. We propose that the magmatic and structural asymmetry observed between these two conjugate margins is consistent with an early rifting phase dominated by simple shear rather than pure
shear deformation. In such a setting Labrador would be the lower plate margin to the southwest Greenland upper plate.

KeywordsLabrador sea; ocean basin; Canada; Greenland
Year2016
JournalGeosphere
PublisherThe Geological Society of America
ISSN1553040X
Digital Object Identifier (DOI)https://doi.org/10.1130/GES01341.1
Web address (URL)http://hdl.handle.net/10545/624259
hdl:10545/624259
Publication dates29 Sep 2016
Publication process dates
Deposited28 Oct 2019, 09:53
Accepted24 Aug 2016
ContributorsDurham University and Shell International
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File Access Level
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