Thermochronology data from Pearya Terrane, Ellesmere Island, North Canadian Margin

Thermochronology data suggest Eocene high-latitude rapid exhumation and topography formation. Enhanced exhumation of northern Ellesmere Island occurred ~67-59 Ma, ~55-48 Ma, 44-38 Ma, and 34-26 Ma. These exhumation periods largely correlate with changes of spreading rates and movement directions of...

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Bibliographic Details
Main Authors: Vamvaka, Agni, Pross, Jörg, Monien, Patrick, Piepjohn, Karsten, Estrada, Solveig, Lisker, Frank, Spiegel, Cornelia
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
apatite fission track and (U-Th)/He thermochronology
Canadian High Arctic
Ellesmere Island
Eurekan orogeny
Pearya Terrane
Arctic
Fram Strait
glacier
Greenland
Greenland Sea
Svalbard
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.905014
https://doi.org/10.1594/PANGAEA.905014
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Summary:Thermochronology data suggest Eocene high-latitude rapid exhumation and topography formation. Enhanced exhumation of northern Ellesmere Island occurred ~67-59 Ma, ~55-48 Ma, 44-38 Ma, and 34-26 Ma. These exhumation periods largely correlate with changes of spreading rates and movement directions of the Norwegian-Greenland Sea. Main topographic growth along the Eurekan belt was temporally coincident with deposition of ice-rafted debris off eastern Greenland. We suggest that Eurekan topography growth was an important trigger for glacier formation in Greenland. Exhumation of northern Ellesmere Island was episodic and was presumably controlled by strike-slip movements along the De Geer Fracture Zone between Svalbard and Greenland. The cessation of rapid exhumation at ~26 Ma can be explained by continental separation between Greenland and Svalbard, which decoupled northern Ellesmere Island from strike-slip movements along the De Geer Fracture Zone, eventually leading to the opening of the Fram Strait.

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