Mercedes Vázquez-Vílchez

ORCID: 0000-0003-4433-5112
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About
Contact & Profiles
Research Areas
  • Geological and Geophysical Studies Worldwide
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • Geology and Paleoclimatology Research
  • Environmental Education and Sustainability
  • Building materials and conservation
  • Archaeological and Geological Studies
  • Educational Games and Gamification
  • Clay minerals and soil interactions
  • Cultural Heritage Materials Analysis
  • Iron oxide chemistry and applications
  • Geography Education and Pedagogy
  • Archaeological and Historical Studies
  • Medieval Architecture and Archaeology
  • E-Learning and Knowledge Management
  • Geological and Tectonic Studies in Latin America
  • Educational Research and Science Teaching
  • Knowledge Societies in the 21st Century
  • Creativity in Education and Neuroscience
  • Recycling and utilization of industrial and municipal waste in materials production
  • Impact of AI and Big Data on Business and Society
  • Educational Innovations and Technology
  • Coastal wetland ecosystem dynamics
  • Spatial Cognition and Navigation
  • Science Education and Pedagogy

Universidad de Granada
2009-2024

Departamento de Educación
2019

Universidad de Valladolid
2018

University of Chile
2013-2016

Mohammed V University
2013

University of Aveiro
2006-2007

Universidad de Jaén
2003-2004

Terra Nova, 23, 257–263, 2011 Abstract New apatite (U‐Th)/He and fission‐track data from the Nevado–Filábride complex in Sierra Nevada of southern Spain are used to constrain Neogene exhumation history. Apatite ages close western indicating that rapid cooling occurred at 8–6 Ma, consistent with due extension along Mecina Fault. The de los Filabres cooled rapidly c . 12 while central experienced less 8 Ma. age distribution can be explained by flexural uplift south‐west footwall lower rates...

10.1111/j.1365-3121.2011.01007.x article EN Terra Nova 2011-06-07

Terra Nova, 24, 505–512, 2012 Abstract The subducted North Maghrebian passive margin was exhumed in the Tortonian (11–7 Ma) by an upper‐crustal brittle‐ductile extensional detachment and brittle low‐angle normal faults a continental subduction transform setting. Temsamane eastern Rif is defined ductile shear zone approximately 100‐m thick with ramp geometry that cuts down into fold‐nappe stack. shows south‐westward kinematics separates lower‐greenschist (≈400 °C) metapelites of units below...

10.1111/j.1365-3121.2012.01089.x article EN Terra Nova 2012-08-08

This paper explores the value of cooperative games in enhancing knowledge and generating pro-environmental engagement students. For this, an educational board game related to global change was developed, validated, subsequently evaluated using future primary school teachers. The validated two phases. Phase I (validation phase): students pursuing a Master’s Degree Secondary Education different aspects game, providing feedback that improved design playing rules. II (implementation–evaluation...

10.3390/educsci11110691 article EN cc-by Education Sciences 2021-10-29

INTRODUCCIÓN. En el presente artículo se presenta una revisión de la literatura indexada en las bases datos Scopus y Web of Science-Clarivate basada análisis indicadores bibliométricos sobre uso tecnologías emergentes educación. Para ello consideran recogidas informe Horizon Report: K-12 Edition: a) espacios maker, b) robótica, c) analíticas, d) realidad virtual, e) inteligencia artificial f) internet cosas (IoT). Además, considera como variable que sean utilizadas enseñanza educación...

10.13042/bordon.2022.94198 article ES cc-by-nc Bordón Revista de Pedagogía 2022-12-20

The distribution pattern of diagenetic conditions to very low-grade metamorphism in the eastern Rif has been determined based on a study clay-mineral assemblages and illite crystallinity Mesozoic metapelites. Low-grade were reached marbles also Beni-Malek serpentinites, as suggested by mineral present antigorite growth serpentinites. Previous thermochronological data are i) 40Ar/39Ar amphiboles from greenschists, ii) K/Ar white micas metasandstones, iii) fission tracks apatites zircons...

10.1344/105.000001843 article EN Geologica Acta 2013-01-01

Abstract We have carried out optical microscopy, X-ray diffraction (XRD) and scanning transmission electron microscopy (SEM TEM) studies of phyllosilicates from black slates very low to low-grade metamorphism. Such belong a Middle/Late Devonian basin an Early Carboniferous associated with the Porto–Tomar–Ferreira do Alentejo strike-slip shear zone (Ossa-Morena Zone, Portuguese Iberian Variscan Massif). These are imbricated in Upper Proterozoic substratum higher metamorphic grade. Kübler...

10.1180/claymin.2007.042.1.08 article EN Clay Minerals 2007-03-01

Abstract. This study focuses on exploring the potential of serious games for improving disaster risk management. The research involves methodological triangulation, analysing and comparing data from content analysis (6 digital games: 3 mobile apps online games), focus groups with experts literature review. results show that only fulfil fundamental narrative indicated by experts, focusing their gameplay more interaction. Such interaction could enhance playful aspect game thus increase desire...

10.5194/egusphere-2024-994 preprint EN cc-by 2024-04-16

sin fines de lucro, desarrollado bajo la iniciativa acceso abierto Fundamentos y líneas trabajo

10.25267/rev_eureka_ensen_divulg_cienc.2022.v19.i1.1103 article ES cc-by-nc-nd Revista eureka sobre enseñanza y divulgación de las ciencias 2022-01-01

The suitability of Triassic Red Beds from northern Jaén in the production structural clay products has been evaluated. These materials have high phyllosilicate contents (36-69%), although some samples are enriched quartz (

10.3989/mc.2004.v54.i273.219 article EN cc-by Materiales de Construcción 2004-03-30

This paper assesses the aptness of Carbonero Formation (in Spanish province Jaén) marls for manufacture high added value ceramic construction materials. Lithologically speaking, comprises three members: a) a marly lower member; b) radiolaritic middle and c) turbiditic upper member. The samples studied were rich in phyllosilicates (> 39%) calcite. quartz feldspar contents low (< 27%). majority illite-smectite mixed layers (14-50%) illite (32-74%). Kaolinite, chlorite palygorskite also...

10.3989/mc.2009.40707 article EN cc-by Materiales de Construcción 2009-05-21
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