ORCID Profile
0000-0003-3410-0344
Current Organisation
Utrecht University
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Publisher: Elsevier BV
Date: 03-2012
Publisher: Elsevier BV
Date: 08-2011
Publisher: Wiley
Date: 02-2010
Publisher: American Geophysical Union (AGU)
Date: 30-04-2020
DOI: 10.1029/2020GL087484
Publisher: Elsevier BV
Date: 10-2010
Publisher: Elsevier BV
Date: 05-2017
Publisher: Elsevier BV
Date: 02-2015
Publisher: Elsevier BV
Date: 08-2010
Publisher: Elsevier BV
Date: 06-2017
Publisher: American Geophysical Union (AGU)
Date: 14-07-2012
DOI: 10.1029/2012TC003144
Publisher: American Geophysical Union (AGU)
Date: 08-2022
DOI: 10.1029/2021TC006922
Abstract: The high‐pressure metamorphic Nevado‐Filábride Complex (NFC) in the Betics mountain range of southeastern Spain exhibits continental and ocean‐derived tectonic units, which are key for understanding the geodynamic evolution of the Western Mediterranean. We address the current debate in the definition of tectonic units, the emplacement of (ultra)mafic rocks, and the timing of burial metamorphism by conducting a structural study combined with single grain fusion 40 Ar/ 39 Ar dating of white micas in structurally critical outcrops of the eastern Sierra de Los Filábres. One older 40 Ar/ 39 Ar age population (38–27 Ma) is found at distance from the main shear zones in the relics of an early foliation, while a younger 40 Ar/ 39 Ar population (22–12 Ma) is dominant in the vicinity of these shear zones, where the early foliation is obliterated. Both age groups are interpreted as the record of deformation or fluid‐induced recrystallization during distinct fabric‐forming events, while alternative scenarios are discussed. A key observation is the presence of an ophiolitic mélange, which—together with new and published geochronological data—allows for a new tectonic hypothesis. This considers Paleogene subduction beneath a Jurassic oceanic lithosphere, followed by the continued subduction of NFC and overlying ophiolites below the Alpujárride Complex. Exhumation during westward slab roll‐back led to the formation of an extensional detachment system that obliquely cut nappe contacts. Although the timing constraints for high pressure‐low temperature (HP‐LT) metamorphism in the NFC remain inconclusive, the new tectonic hypothesis provides a solution that can account for both Paleogene and Miocene ages of HP‐LT metamorphism.
Publisher: American Geophysical Union (AGU)
Date: 06-2014
DOI: 10.1002/2014GC005294
Publisher: American Geophysical Union (AGU)
Date: 12-2008
DOI: 10.1029/2008GC002127
Publisher: Oxford University Press (OUP)
Date: 04-2008
Publisher: American Geophysical Union (AGU)
Date: 08-2010
DOI: 10.1029/2009TC002620
Publisher: IGI Global
Date: 2007
DOI: 10.4018/978-1-59904-304-3.CH015
Abstract: simSchool is a game-based simulation developed with funding from the Preparing Tomorrow’s Teachers to Use Technology (PT3, 2003) program of the United States Department of Education. The simulation provides users with a training environment for developing skills such as lesson planning, differentiating instruction, classroom management, special education, and adapting teaching to multiple cognitive abilities. This chapter uses simSchool as an ex le to present and discuss an application of the Conceptual Assessment Framework (CAF) of (Almond, Steinberg, & Mislevy, 2002) as a general model for building assessments of what users learn through games and simulations. The CAF organizes the theories of teaching as well as the inferential frameworks in simSchool that are used to provide feedback to players about their levels of knowledge and abilities as teachers. The framework is generally relevant and useful for planning how to assess gains made by users while playing games or using simulations.
No related grants have been discovered for Douwe van Hinsbergen.