Zobrazeno 1 - 10
of 117
pro vyhledávání: '"Vissers, R.L.M."'
Autor:
Vissers, R.L.M., Meijer, P.Th.
Publikováno v:
In Earth-Science Reviews August 2012 114(1-2):61-83
Publikováno v:
In Earth and Planetary Science Letters 30 March 2004 220(1-2):185-199
The Pyrenees at the Iberia–Europe collision zone contain sediments showing Albian–Cenomanian high-temperature metamorphism, and coeval alkaline magmatic rocks. Stemming from different views on Jurassic–Cretaceous Iberian microplate kinematics,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::bb76992b45daa1e9e6aa9fbe4db71ab9
https://dspace.library.uu.nl/handle/1874/335478
https://dspace.library.uu.nl/handle/1874/335478
Autor:
Van Hinsbergen, D.J.J., Maffione, M., Plunder, A., Kaymakçi, N., Ganerød, M., Hendriks, B.W.H., Corfu, F., Gürer, D., de Gelder, G.I.N.O., Peters, K., McPhee, P.J., Brouwer, Fraukje M., Advokaat, E.L., Vissers, R.L.M., NWO-VIDI: Subduction iniation reconstructed from Neotethyan kinematics (SINK): an integrated geological and numerical study of the driving forces behind plate tectonics, ERC-SINK: Subduction Initiation reconstructed from Neotethyan Kinematics, Mantle dynamics & theoretical geophysics, Paleomagnetism, Structural geology and EM
Publikováno v:
Tectonics, 35(4), 983. Wiley
In Central and Western Anatolia two continent-derived massifs simultaneously underthrusted an oceanic lithosphere in the Cretaceous and ended up with very contrasting metamorphic grades: high pressure, low temperature in the Tavşanlı zone and the l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::93f12f954bc8ca3995972b19340e0db4
https://dspace.library.uu.nl/handle/1874/335960
https://dspace.library.uu.nl/handle/1874/335960
Autor:
Advokaat, Eldert, van Hinsbergen, D.J.J., Maffione, M., Langereis, C.G., Vissers, R.L.M., Cherchi, A., Schroeder, R., Madani, H., Columbu, S.
Key to understanding the complex Mediterranean subduction history is the kinematic reconstruction of its paleogeography after Jurassic extension between Iberia, Eurasia, and Africa. While post-Eocene Liguro-Provençal back-arc extension, and associat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::48743d5c0d155ad138fd607561131622
https://dspace.library.uu.nl/handle/1874/301064
https://dspace.library.uu.nl/handle/1874/301064
The western Mediterranean recorded subduction rollback, slab segmentation and separation. Here we address the questions of what caused Oligocene rollback initiation, and how its subsequent evolution split up an originally coherent fore arc into circu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::850ad02f53083fc85652793040a3ea7f
https://dspace.library.uu.nl/handle/1874/310136
https://dspace.library.uu.nl/handle/1874/310136
Publikováno v:
In Earth and Planetary Science Letters September 2012 345-348:60-71
Publikováno v:
American Geophysical Union (AGU) Fall Meeting.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=erc_________::bf3dbcdf3c4db6c39658bf32c615665c
Autor:
Vissers, R.L.M.
Publikováno v:
Geologica Belgica, 15(1-2), 53
The Betic Cordillera of southern Spain forms a clear example of a collisional orogen that has undergone large-scale late-orogenic extension while convergent motion of the bounding plates continued. The orogen provides a unique opportunity to study th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2afaba06f29a3e2065db78e79a351da3
https://dspace.library.uu.nl/handle/1874/258646
https://dspace.library.uu.nl/handle/1874/258646