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Bliekendaal, Erik (author)A extensive overview of the literature discussion on magma chamber evolution is presented. There are two end-member models, the large magma chamber and the incremental pluton growth. This author considers both models for valid and concludes that only detailed study of a pluton can reveal to what extent which model is most plausible. From field...report 2012
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Ruiter, A (author)The development and occurrence of closed circular depressions in the Netherlands and Germany is still a point of uncertainty. Whether these depressions are pingo remnants or formed by other processes is important to know before using these depression as pingos in reconstructions of past climate conditions. More insight in the occurrence of these...report 2012
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Slootman, A. (author)The Pleistocene biocalcarenite complex of Favignana Island consists of coarse-grained, resedimented cool-water carbonate sands composed of skeletal debris of red algae, bryozoans, echinoids, foraminifera, bivalves and rhodoids. Dozens of excellent exposures of the Favignana Calcarenite encompass sedimentary structures which originated from the...report 2012
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- van Lipzig, M.L.H.M. (author) report 2011
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Koopman, Marijn (author)The Ilgin Basin in Central Anatolia is the southeastern extension of the Akşehir-Afyon Basin, situated at the eastern periphery of the Isparta Angle region. The basin geometry, its patterns of sediment infill and its kinematics are controlled by the interference between Late Cenozoic (i.e. neotectonic) overprints and re-activation of old,...report 2011
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- Dijkhuizen, Anja (author) report 2011
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Grothe, Arjen (author)Upper Cretaceous and Paleogene sediments in the Tarim Basin (western China) are archive of the easternmost remnants of the early Paratethys Sea, an epicontinental sea that covered a large part of Eurasia and probably extended into the Mediterranean Tethys in the west. Its final retreat out of the Tarim Basin has been suggested to be associated...report 2011
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- van Rossem, Lisa (author) report 2011
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Klaver, Martijn (author)The Bakhuis granulite belt (western Suriname) consists of an early Proterozoic high-grade supracrustal sequence characterised by ubiquitous compositional banding. Orthopyroxene is invariably present in both the mafic and dominant quartzofeldspathic lithologies. Locally, the Bakhuis belt has experienced ultrahigh-temperature metamorphic...report 2011
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Karimlou, Gosro (author)The impact of an abandoned hydraulic gold mine and an open cast copper-gold mine on the quality of fine-grained sediment (<63 μm) was investigated at several creeks in the Quesnel river catchment catchment in British Columbia, Canada. Bed sediment samples, suspended sediment samples, vertical profiles and/or corings were collected at five field...report 2011
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Klompmaker, A.A. (author), Artal, P. (author), Gulisano, G. (author)The crab genus Rathhunopon is exclusively known from Cretaceous rocks, mainly from Europe. Here two new European localities are presented: one in the Albian/Cenomanian of northern Spain yielding well-preserved specimens of Rathhunopon ohesum, and one from the lower Aptian at the German-Austrian border yielding Rathhunopon schrattenkalkensis n....report 2011
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Klompmaker, A.A. (author), Artal, P. (author), Fraaije, R.H.B. (author), Jagt, J.W.M. (author)Representatives of the family Gastrodoridae were exclusively known from Jurassic deposits in central Europe. Here, the first Cretaceous species, Gastrodorus cretahispanicus n. sp., is recorded from reefal strata of the Eguino Formation (Albeniz Unit) of Albian-Cenomanian age, in western Navarra (northern Spain). Not only does the occurrence of...report 2011
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Verbaas, J. (author)The Friningen Peridotite Lens, found in N. Jämtland, Central Sweden is a tectonically emplaced garnet peridotite lens located in the Seve Nappe Complex (SNC) of the Scandinavian Caledonides. The peridotite records older protolith mineral assemblages than the host gneisses and is crosscut by a basic garnet pyroxenite dike. Metamorphism in the SNC...report 2011
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- Li, J. (author), Menenti, M. (author), Donselaar, M.E. (author), Prins, M.A. (author), Hosseini Aria, S.E. (author), Koenders, R. (author), Oyes, A. (author) report 2011
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Polling, M. (author)The early Eocene (59-52 Ma) is a period in which Earth’s climate underwent gradual warming that was interrupted by several transient extreme warming events termed ‘hyperthermals’. The major hyperthermals ‐ the PETM (~55.5 Ma) and the ETM2 (~53.6 Ma) – are accompanied By 4-8ºC warming, massive release of 13C depleted carbon into the ocean...report 2011
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Schoffelen, N. (author)East Antarctica is covered by the East Antarctic Ice Sheet (EAIS) that stretches from the Centre of the continent to the coastline and holds more than three quarters of all the ice on the globe today. The East Antarctic coastline is characterised by glaciers that rise up hundreds of meters Above sea level and confine the boundary between the ice...report 2011
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- Li, J. (author), Donselaar, M.E. (author), Bloemsma, Mr> (author), Prins, M.A. (author), Weltje, G.J. (author), Torres, Y.A. (author) report 2011
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Kil, R.A. (author)The island of Favignana provides an exceptional three-dimensional insight in the architecture of a Lower Pleistocene bioclastic calcarenite complex. Due to the degree of quarrying, a large amount of outcrops is available in the eastern part of the island. Two campaigns resulted in the logging of stratigraphic sections, recording of sedimentary...report 2010
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de Haas, Tjalling (author)The upper Columbia River is an anastomosing river. Anastomosing rivers consist of a network of channels enclosing floodbasins. The factors that determine the configuration of river networks such as the upper Columbia River are unknown. Additionally the origin of anastomosing rivers is unclear. Two main theories exist on the origin of anastomosis...report 2010
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- Lavooi, Eva (author) report 2010