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Curved orogenic belts, back-arc basins, and obduction as consequences of collision at irregular continental margins (2021)
Journal Article
Schliffke, N., van Hunen, J., Gueydan, F., Magni, V., & Allen, M. B. (2021). Curved orogenic belts, back-arc basins, and obduction as consequences of collision at irregular continental margins. Geology, 49(12), 1436-1440. https://doi.org/10.1130/g48919.1

Continental collisions commonly involve highly curved passive plate margins, leading to diachronous continental subduction during trench rollback. Such systems may feature backarc extension and ophiolite obduction postdating initial collision. Modern... Read More about Curved orogenic belts, back-arc basins, and obduction as consequences of collision at irregular continental margins.

The Role of Crustal Buoyancy in the Generation and Emplacement of Magmatism During Continental Collision (2019)
Journal Article
Schliffke, N., Hunen, J., Magni, V., & Allen, M. B. (2019). The Role of Crustal Buoyancy in the Generation and Emplacement of Magmatism During Continental Collision. Geochemistry, Geophysics, Geosystems, 20(11), 4693-4709. https://doi.org/10.1029/2019gc008590

During continental collision, considerable amounts of buoyant continental crust subduct to depth and subsequently exhume. Whether various exhumation paths contribute to contrasting styles of magmatism across modern collision zones is unclear. Here we... Read More about The Role of Crustal Buoyancy in the Generation and Emplacement of Magmatism During Continental Collision.