Tectonic evolution of northern Ellesmere Island: insights from the Pearya Terrane, Ellesmerian Clastic Wedge And Sverdrup Basin
The tectonic evolution of northern Ellesmere Island is dominated by the accretion of the Pearya Terrane and the progressive reworking of materials from the Pearya Terrane and the northern Caledonides. Geochronology from a suite of seven Succession I orthogneiss samples defines a range of earliest Ne...
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| Format: | Others |
| Language: | English |
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University of Iowa
2012
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| Online Access: | https://ir.uiowa.edu/etd/3496 https://ir.uiowa.edu/cgi/viewcontent.cgi?article=3497&context=etd |