Zobrazeno 1 - 9
of 9
pro vyhledávání: '"D. J. J. van Hinsbergen"'
Publikováno v:
Solid Earth, Vol 9, Pp 759-776 (2018)
The geotherm in subduction zones is thought to vary as a function of the subduction rate and the age of the subducting lithosphere. Along a single subduction zone the rate of subduction may strongly vary due to changes in the angle between the tre
Externí odkaz:
https://doaj.org/article/4b05dca571d644299764686ff4ed3eec
Autor:
D. Gürer, D. J. J. van Hinsbergen, M. Özkaptan, I. Creton, M. R. Koymans, A. Cascella, C. G. Langereis
Publikováno v:
Solid Earth, Vol 9, Pp 295-322 (2018)
To quantitatively reconstruct the kinematic evolution of Central and Eastern Anatolia within the framework of Neotethyan subduction accommodating Africa–Eurasia convergence, we paleomagnetically assess the timing and amount of vertical axis rotatio
Externí odkaz:
https://doaj.org/article/7bdce8a1ded64aaa863c1515b4086c6a
Autor:
M. Baatsen, D. J. J. van Hinsbergen, A. S. von der Heydt, H. A. Dijkstra, A. Sluijs, H. A. Abels, P. K. Bijl
Publikováno v:
Climate of the Past, Vol 12, Iss 8, Pp 1635-1644 (2016)
Studies on the palaeoclimate and palaeoceanography using numerical model simulations may be considerably dependent on the implemented geographical reconstruction. Because building the palaeogeographic datasets for these models is often a time-consumi
Externí odkaz:
https://doaj.org/article/82e7fdce6d004df9a98cd407f65e1e64
Autor:
G. Hoareau, B. Bomou, D. J. J. van Hinsbergen, N. Carry, D. Marquer, Y. Donnadieu, G. Le Hir, B. Vrielynck, A.-V. Walter-Simonnet
Publikováno v:
Climate of the Past, Vol 11, Iss 12, Pp 1751-1767 (2015)
The 58–51 Ma interval was characterized by a long-term increase of global temperatures (+4 to +6 °C) up to the Early Eocene Climate Optimum (EECO, 52.9–50.7 Ma), the warmest interval of the Cenozoic. It was recently suggested that sustained high
Externí odkaz:
https://doaj.org/article/2e03d08802c841dca0e62f2ccc46bf17
Autor:
D. J. J. van Hinsbergen, M. Mensink, C. G. Langereis, M. Maffione, L. Spalluto, M. Tropeano, L. Sabato
Publikováno v:
Solid Earth, Vol 5, Iss 2, Pp 611-629 (2014)
The first and foremost boundary condition for kinematic reconstructions of the Mediterranean region is the relative motion between Africa and Eurasia, constrained through reconstructions of the Atlantic Ocean. The Adria continental block is in a down
Externí odkaz:
https://doaj.org/article/294eee30b19548faa019cb2093950f47
Publikováno v:
International Journal of Earth Sciences. 95:463-490
Following an Early Miocene phase of N–S extension affecting the entire Hellenides, 50° clockwise rotation affected western Greece. Modern GPS analyses show rapid southwestward motion in southwestern Greece over subducting oceanic lithosphere and n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e858fde6e5496a70b9fc53d65d1d3673
https://doi.org/10.1007/s00531-005-0047-5
https://doi.org/10.1007/s00531-005-0047-5
Publikováno v:
EOS, Transactions, American Geophysical Union, Fall Meeting Suppl. 91
AGU 2010 Fall Meeting (San Francisco 2010)#
AGU 2010 Fall Meeting (San Francisco 2010)#
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0f068d84d31d9ea98fefa11a79146d35
https://gfzpublic.gfz-potsdam.de/pubman/item/item_244224
https://gfzpublic.gfz-potsdam.de/pubman/item/item_244224
Publikováno v:
Tectonics. 24
[1] After their emplacement in the course of the late Mesozoic and the Cenozoic, the Hellenic nappes became fragmented during late orogenic extension since the late Eocene. Here we focus on the transition of underthrusting during nappe emplacement to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::716083dd9e1bbc5129b0470e8a700c0c
https://doi.org/10.1029/2004tc001692
https://doi.org/10.1029/2004tc001692
The Apennine belt represents a typical orogenic segment of the western Mediterranean, characterized by the tectonic convergence between European and Africa plates after oceanic subduction. Both oceanic- and continent-derived metamorphic complexes, co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::72358003a9886a33b67cbc8aa6a0ad85
http://hdl.handle.net/11585/661096
http://hdl.handle.net/11585/661096