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New: Paper in Nature Geoscience!

New: Fieldwork photos Namibia 2009

 

 

Last update:  Decenber 22, 2009


Dr. Douwe J.J. van Hinsbergen
Center for Physics of Geological Processes, Oslo

postal address
Center for Physics of Geological Processes
University of Oslo
Sem Sælands vei 24
0316  Oslo
Norway
e-mail: douwework@gmail.com

 

                                

 

Bizarre erosional camel near Kula - western Turkey

 

 

Research interest:

I currently work as Post-Doc at the University of Oslo, working with Trond Torsvik, and construct plate tectonic restorations of mountain belts at subduction zones. In particular I reconstruct the Tethyan Realm, which was a large, triangular ocean with multiple small continental blocks, that during the last 150 or 200 million years or so closed between Africa, Arabia, India and Australia in the south, and Eurasia in the north. Its closure led to the formation of the Alpine-Himalayan mountain belt and (part of) the Indonesian archipelago, stretching from the Pyrenees in the west, to Papua New Guinnee in the east.

This mountain belt consists of geological elements (folded and thrusted rock slices) that were scraped off when the Tethyan lithosphere subducted below Eurasia. I try to place all the geological elements we find in this enormous mountain belt back into their original, pre-subduction position (based on geological techniques from e.g. structural geology and paleomagnetism), and then link these reconstructions to mantle structure that we know from seismic tomography, to locate the subducted, disappeared lithosphere in the mantle. This way we can make 4D plate reconstructions, and reconstruct not only the surface, but also the mantle structure through time.

In particular, this work is carried out in the following regions:

Mediterranean

The Mediterranean region is one of the most geologically complex regions in the world, with currently narrow subduction zones (e.g. in the Betic-Rif, the Alps, the Apennines, the Dinarids, the Carpathians, the Aegean and the Cyprus segments) that subduct in practically every thinkable direction. The reconstruction of this region is therefore complex, but very important, because all these subduction zones anchor Europe firmly to the mantle. And because Europa, or rather Eurasia, is connected to all other plates, we can here define the position of all plates to the mantle in a slab-based mantle reference frame (see Nature Geoscience paper of Douwe van der Meer et al).

My work has been focused so far in Greece, Bulgaria, Turkey, Ukraine and Spain and will continue the next years to cover the entire system. This work includes PhD projects under my co-supervision of Côme Lefebvre, Maud Meijers, Ayten Koç and Ahmet Peynircioğlu.

India-Asia collision

I carried out a post-doc at the University of Leicester with Dickson Cunningham, UK, in 2004-2006, working in the Gobi Altai region in southern Mongolia, which is a strike-slip belt that formed in the Neogene as a far-field expression of the India-Asia collision. After that project, I was invited by my friend and colleague Guillaume-Dupont-Nivet to combine my paleomagnetic data from Mongolia with his results from Tibet, to start working on a paleomagnetic study constraining the distribution of deformation in Asia and India as a result of this collision. This collaboration has proven to be very fruitful, and current research is focusing on a complete reconstruction of the collision from paleomagnetic, structural and seismic tomographic constraints, also collaborating with Wim Spakman, Paul Kapp, Pete Lippert and Pavel Doubrovine.

Timor and the Banda Arc

Starting in the spring of 2010, I will participate in a collaborative project funded by the NSF that will focus on the accretionary history of the island of Timor in SE Indonesia, during arc-continent collision between the Australian continent and the oceanic Banda plate. This work will likely expand into a detailed geological reconstruction of the Banda Arc, and occurs in collaboration with Nadine McQuarrie and Garrett Tate (both Princeton) and Ron Harris (Brigham Young).

Caribbean

Since 2007, I have worked in the Caribbean region, reconstructing the arc-continent collision of Cuba and the triple-junction processes at the North-American – Caribbean – Pacific plate junction by doing paleomagnetic research in the Chortis Block of Honduras, in collaboration with Manuel Iturralde-Vinent, Antonio Garcia-Casco, Rob Rogers and Roberto Molina-Garza.