PhD geology student. My main PhD topic is related to the degasssing mechanisms characterization of Deception Island volcano (Antarctica) through Noble gas and Stable Isotope (H and O) geochemistry.
I am a very hardworking person, always motivated and looking forward to opportunities as they arise. My strengths are punctuality, persistence and ethical standards.
-International group workshops (Students from France, UK, Greece, Italy and Perú) -Virtual Reality workshops (Isle of Wight, Metaxa Mine, Puy de Lémptegy) -Landslides (Isle of Wight, UK), Volcanic risk and hazards (Iceland, Santorini) and Geoheritage (France) -Preparation of Presentations -ArcGIS Story Maps Introduction -Assistance to Puy de Lémptegy living tour recording
Rise of magmas and eruption
Physical Magmatology Magma’s sources and differentiation mechanisms
Digital Modelling Geological mapping in volcanic fields
Subsurface Geophysics Imagery and Remote Sensing
Analytical Techniques
Master Thesis:
Álvarez-Valero. A, Gisbert. G, Aulinas. M, Geyer. A, Kereszturi. G, Polo Sánchez. A, Núñez Guerrero. E, Sumino. H, (2020). δD and δO evolution under Deception Island volcano (Antarctica): Implications for magma ascent and eruption forecasting. Chemical Geology. 119595. https://doi.org/10.1016/j.chemgeo.2020.119595
Álvarez-Valero. A, Aulinas. M, Geyer. A, Gisbert. G, Kereszturi. G, Núñez Guerrero. E, Polo Sánchez. A, Sumino. H, (2020). Magma ascent and eruption forecasting at Deception Island volcano (Antarctica) evidenced by δD and δ18O variations. EGU General Assembly. Submission EGU2020-12700. https://doi.org/10.5194/egusphere-egu2020-12700
Voluntary training in the field of metamorphic petrology in the south-east of Salamanca province (Map Sheet MAGNA 1.50000 Nº529), especially in the vicinities of Bercimuelle, Puente del Congosto, Gallegos de Solmirón and El Mirón. This training was realised in rocks that belong to the Esquisto-Grauvaquico Complex, dated Pre-Ordovicien, who suffered metamorphic procceses associated to Variscan Orogeny and Pre, Sin or Post-Variscan igneous intrusions.