Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Alexander J P, Houben"'
Autor:
B. Jaarsma, Renaud Bouroullec, J.M. Verweij, S. Nelskamp, J.C. Doornenbal, Geert-Jan Vis, C.R. Geel, J. Juez-Larre, H.F. Mijnlieff, M. M. ter Borgh, Alexander J. P. Houben, H. Kombrink, G. de Bruin, J.H. ten Veen, R.A.F. Dalman, K. van Ojik, R.M.C.H. Verreussel, M. Kortekaas, T.C. Pharaoh
Publikováno v:
Geological Society, London, Special Publications. 494:233-268
The Southern North Sea Basin area, stretching from the UK to the Netherlands, has a rich hydrocarbon exploration and production history. The past, present and expected future hydrocarbon and geothermal exploration trends in this area are discussed fo
Autor:
Alexander J. P. Houben, Geert-Jan Vis
Publikováno v:
Netherlands Journal of Geosciences. 100
Knowledge of the stratigraphic development of pre-Carboniferous strata in the subsurface of the Netherlands is very limited, leaving the lithostratigraphic nomenclature for this time interval informal. In two wells from the southwestern Netherlands,
Autor:
Francesca Sangiorgi, Francien Peterse, Peter K. Bijl, Stefan Schouten, Ariadna Salabarnada, Alexander J. P. Houben, Henk Brinkhuis, Julian D. Hartman, Carlota Escutia
Publikováno v:
Climate of the Past. 14:1275-1297
The volume of the Antarctic continental ice sheet(s) varied substantially during the Oligocene and Miocene (∼34–5 Ma) from smaller to substantially larger than today, both on million-year and on orbital timescales. However, reproduction through p
Autor:
Alexander J. P. Houben, K. Dybkjaer, C.R. Geel, P. N. Johannessen, Renaud Bouroullec, S.J. Kerstholt-Boegehold, Dirk K. Munsterman, R.M.C.H. Verreussel
Publikováno v:
Geological Society, London, Special Publications. 469:305-340
This paper presents the results of a cross-border study of the Middle Jurassic–Early Cretaceous rift phase in the Danish–German–Dutch Central Graben area. Based on long-distance correlations of palynologically interpreted wells, a stepwise basi
Anoxic sediments as compared to oxic settings encompass a much higher proportion of relatively labile and thus more reactive organic matter, naturally giving rise to condensation reactions (such as vulcanisation) transforming the original biomolecule
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::80905225feef8ed4830d262693a97bee
https://doi.org/10.5194/bg-2019-373
https://doi.org/10.5194/bg-2019-373
Autor:
Howie D. Scher, Vera A. Korasidis, Stephen J. Gallagher, Alexander J. P. Houben, Paul R. Bown, Brian McGowran, Li Qianyu, Bridget S. Wade, Tony Allan, Guy R. Holdgate
Publikováno v:
Global and Planetary Change. 191:103218
Multiple stable isotope investigations from upper Eocene to lower Oligocene deep-water marine sequences record the transition from global greenhouse to the icehouse conditions (Oi-1 glacial). While Southern Ocean high latitude deep sea records of thi
Autor:
Alexander J. P. Houben, Ariadna Salabarnada, Francesca Sangiorgi, Francien Peterse, Stefan Schouten, Peter K. Bijl, Julian D. Hartman, Carlota Escutia
Today, the temperature of the surface waters near the Antarctic coast is a determining factor in the formation of Antarctic Bottom Water (AABW) through sea-ice production, sea-ice extent, and the extent of the ice shelf. For the Oligocene, deep-sea b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53f70d2e2853be507567a85139e500fe
https://doi.org/10.5194/cp-2017-153
https://doi.org/10.5194/cp-2017-153
Autor:
Julian D. Hartman, Francesca Sangiorgi, Ariadna Salabarnada, Francien Peterse, Alexander J. P. Houben, Stefan Schouten, Carlota Escutia, Peter K. Bijl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd099212c18f35cfbc11efe7964e48c9
https://doi.org/10.5194/cp-2017-153-supplement
https://doi.org/10.5194/cp-2017-153-supplement
Autor:
Julian D. Hartman, Carlota Escutia, Peter K. Bijl, Francesca Sangiorgi, Ariadna Salabarnada, Alexander J. P. Houben, Jörg Pross
Next to atmospheric CO2 concentrations, oceanographic conditions are a critical factor determining the stability of Antarctic marine-terminating ice sheets. The Oligocene and Miocene epochs (~ 34–5 Ma) were time intervals with atmospheric CO2 conce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55d00d31ac9496f73d6b964825a32897
https://doi.org/10.5194/cp-2017-148
https://doi.org/10.5194/cp-2017-148
Autor:
Peter K. Bijl, Alexander J. P. Houben, Julian D. Hartman, Jörg Pross, Ariadna Salabarnada, Carlota Escutia, Francesca Sangiorgi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d6345ef2eb918291a33f506ace12ae3
https://doi.org/10.5194/cp-2017-148-supplement
https://doi.org/10.5194/cp-2017-148-supplement