Lithofacies architecture of a proximal ignimbrite: Diego Hernandez Wall, Las Canadas Caldera, Tenerife
Presentation / Conference Contribution
Smith, N., & Kokelaar, P. (2010, January). Lithofacies architecture of a proximal ignimbrite: Diego Hernandez Wall, Las Canadas Caldera, Tenerife. Poster presented at Volcanic and Magmatic Studies Group, Glasgow, Jan 2010
All Outputs (24)
Investigating potential charge mechanisms in the Levantine Basin using 1D basin modelling
Presentation / Conference Contribution
Treloar, M., Dowey, N., & Macgregor, D. (2018, May). Investigating potential charge mechanisms in the Levantine Basin using 1D basin modelling. Paper presented at Eastern Mediterranean – An emerging major petroleum province, Geological Society, London
Near-vent settings and processes of the 273 ka Poris eruption (Tenerife): Ignimbrite deposition, caldera formation and phreatomagmatism
Presentation / Conference Contribution
Smith, N., Kokelaar, B., & Branney, M. (2011, January). Near-vent settings and processes of the 273 ka Poris eruption (Tenerife): Ignimbrite deposition, caldera formation and phreatomagmatism. Paper presented at Volcanic and Magmatic Studies Group Annual Meeting, Cambridge, UK
Near-vent processes of the 273 ka Poris eruption (Tenerife): ignimbrite sedimentation, hybrid deposition and phreatomagmatism
Presentation / Conference Contribution
Smith, N., Kokelaar, B., & Branney, M. (2011, June). Near-vent processes of the 273 ka Poris eruption (Tenerife): ignimbrite sedimentation, hybrid deposition and phreatomagmatism. Paper presented at Earth on the edge: Science for a sustainable planet. International Union of Geodesy and Geophysics, Melbourne, AustraliaThe proximal succession of the 273 ka Poris eruption in the Diego Hernandez wall of Las Cañadas, Tenerife, records opening, main, and waning stages of explosive activity. Stratigraphic and geochemical correlations show varying processes between prox... Read More about Near-vent processes of the 273 ka Poris eruption (Tenerife): ignimbrite sedimentation, hybrid deposition and phreatomagmatism.