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Plate rotation during continental collision and its relationship with the exhumation of UHP metamorphic terranes: Application to the Norwegian Caledonides

Bottrill, A.D.; van Hunen, J; Cuthbert, S.J.; Brueckner, H.K.; Allen, M.B.

Plate rotation during continental collision and its relationship with the exhumation of UHP metamorphic terranes: Application to the Norwegian Caledonides Thumbnail


Authors

A.D. Bottrill

S.J. Cuthbert

H.K. Brueckner



Abstract

Lateral variation and asynchronous onset of collision during the convergence of continents can significantly affect the burial and exhumation of subducted continental crust. Here we use 3-D numerical models for continental collision to discuss how deep burial and exhumation of high and ultrahigh pressure metamorphic (HP/UHP) rocks are enhanced by diachronous collision and the resulting rotation of the colliding plates. Rotation during collision locally favors eduction, the inversion of the subduction, and may explain the discontinuous distribution of ultra-high pressure (UHP) terranes along collision zones. For example, the terminal (Scandian) collision of Baltica and Laurentia, which formed the Scandinavian Caledonides, resulted in the exhumation of only one large HP/UHP terrane, the Western Gneiss Complex (WGC), near the southern end of the collision zone. Rotation of the subducting Baltica plate during collision may provide an explanation for this distribution. We explore this hypothesis by comparing orthogonal and diachronous collision models and conclude that a diachronous collision can transport continental material up to 60 km deeper, and heat material up to 300°C hotter, than an orthogonal collision. Our diachronous collision model predicts that subducted continental margin material returns to the surface only in the region where collision initiated. The diachronous collision model is consistent with petrological and geochonological observations from the WGC and makes predictions for the general evolution of the Scandinavian Caledonides. We propose the collision between Laurentia and Baltica started at the southern end of the collisional zone, and propagated northward. This asymmetric geometry resulted in the counter clockwise rotation of Baltica with respect to Laurentia, consistent with paleomagnetic data from other studies. Our model may have applications to other orogens with regional UHP terranes, such as the Dabie Shan and Papua New Guinea cases, where block rotation during exhumation has also been recorded.

Citation

Bottrill, A., van Hunen, J., Cuthbert, S., Brueckner, H., & Allen, M. (2014). Plate rotation during continental collision and its relationship with the exhumation of UHP metamorphic terranes: Application to the Norwegian Caledonides. Geochemistry, Geophysics, Geosystems, 15(5), 1766-1782. https://doi.org/10.1002/2014gc005253

Journal Article Type Article
Acceptance Date Mar 12, 2014
Online Publication Date May 14, 2014
Publication Date May 14, 2014
Deposit Date Jul 24, 2014
Publicly Available Date Jun 17, 2016
Journal Geochemistry, Geophysics, Geosystems
Publisher American Geophysical Union
Peer Reviewed Peer Reviewed
Volume 15
Issue 5
Pages 1766-1782
DOI https://doi.org/10.1002/2014gc005253

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Published Journal Article (1.7 Mb)
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Copyright Statement
Bottrill, A. D., J. Hunen, S. J. Cuthbert, H. K. Brueckner, and M. B. Allen (2014), Plate rotation during continental collision and its relationship with the exhumation of UHP metamorphic terranes: Application to the Norwegian Caledonides, Geochemistry, Geophysics, Geosystems, 15, 1766–1782, 10.1002/2014GC005253 (DOI). To view the published open abstract, go to http://dx.doi.org and enter the DOI.





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