A5007201898- Geological and Geophysical Studies Worldwide
- Geography Education and Pedagogy
- 3D Surveying and Cultural Heritage
- Geological Modeling and Analysis
- Geotourism and Geoheritage Conservation
- Geological formations and processes
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- Geography and Education Methods
- Medieval Architecture and Archaeology
- Archaeology and Cultural Heritage
- Environmental and Ecological Studies
- Landslides and related hazards
- Archaeological and Historical Studies
- Archaeological and Geological Studies
- Geological and Geochemical Analysis
- Building materials and conservation
Universidad de Oviedo
2018-2022
Abstract. The restrictions implemented to contain the spread of COVID-19 pandemic during 2020 and 2021 have forced university-level educators from around world seek alternatives residential physical field trips that constitute a fundamental pillar Geoscience programmes. field-mapping course for second-year Geology BSc students Cardiff University was replaced with virtual mapping set in same area as previous years, Esla Nappe (Cantabrian Zone, NW Spain). designed aim providing methodology...
Abstract. The restrictions implemented to contain the spread of COVID-19 pandemic during 2020 and 2021 have forced university-level educators from around world seek alternatives residential physical field trips which constitute a fundamental pillar geoscience programmes. field-mapping course for 2nd year Geology BSc students Cardiff University was replaced with virtual mapping set in same area as previous years, Esla Nappe (Cantabrian Zone, NW Spain). designed aim providing methodology...
<p>The Esla Nappe is located in the external foreland and thrust belt of Variscan Orogen NW Iberian Massif (Cantabrian Zone, Iberia). It formed by a near-complete Palaeozoic sedimentary succession. With displacement around 19 km, nappe was emplaced along thin (<2–3 m) basal shear zone (ENBSZ) at an estimated minimum depth 4 km. Emplacement took place during Moscovian (ca. 312 Ma). Fault-rock assemblages record variety alternating deformation mechanisms...
<p>The size and shape of rock constituent particles can provide substantial information about the environment in which rocks are formed also their evolution during geological history. There several processes that generate specific particle shapes. We focus on three effects as end members: sediment transport water producing sub-rounded particles, tectonic fracturing angular fragments chemical corrosion at grain boundaries increasing rugosity. In this work we test morphological...
<p>The isotopic carbon and oxygen isotope composition of carbonates (δ<sup>13</sup>C δ<sup>18</sup>O), determined by temperature the relative abundances stable isotopes both elements in water at time carbonate is precipitated, can be modified subsequently during geological processes that involve recrystallization carbonate. Temperature changes mostly affect...
<p>The Esla Nappe is located in the foreland and thrust belt of Variscan Orogen (Cantabrian Zone, NW Iberia). It formed by a near-complete Palaeozoic sedimentary succession. With displacement around 19 km, nappe was emplaced along thin (<2–3 m) basal shear zone (ENSZ) at minimum depth 4 km during Moscovian (ca. 312 Ma). Fault-rock assemblages record variety alternating deformation mechanisms processes, including cataclastic flow, pressure solution...