Research paperGeophysical evidence for temporal and structural relationships within the monogenetic basalt volcanoes of the Auckland volcanic field, northern New Zealand
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The interplay between environmental and magmatic conditions in eruption style transitions within a fissure-aligned monogenetic volcanic system of Auckland, New Zealand
2022, Journal of Volcanology and Geothermal ResearchCitation Excerpt :This indicates a combination of the diminishing of external water sources to sustain phreatomagmatic activity and a likely increase in magma flux and potential lining of conduit walls by chilled magma, evidenced by the large volume of lava production in the final stage of the eruption (e.g., Head and Wilson, 1989). The scoria cone deposits were partially covered (Searle, 1961; Rout et al., 1993) (Fig. 5a), along with all the underlying tuff rings (Firth, 1930) (Fig. 5c), by alternating agglutinated lava spatter forming some clastogenic flows and rubbly pahoehoe to a'a lava flows (Facies SAF, Fig. 6), which eventually became the dominant deposit produced, flowing over the tuff ring and beyond to the north and west (Figs. 5b, 9a, 10h). Where the lava and spatter covered the tuff rings, the tuff was baked and subsequently formed an altered rim (Fig. 4b).
El Estribo Volcanic Complex: Evolution from a shield volcano to a cinder cone, Pátzcuaro Lake, Michoacán, México
2015, Journal of Volcanology and Geothermal ResearchA geophysical comparison of the diatremes of simple and complex maar volcanoes, Newer Volcanics Province, south-eastern Australia
2014, Journal of Volcanology and Geothermal ResearchCitation Excerpt :Therefore the only way to image the structure of the diatreme and gain a greater understanding of the volcanoes eruptive histories is to use geophysical techniques (Blaikie et al., 2012). The application of geophysical techniques to understand the subsurface morphology of maar volcanoes has become increasingly common (e.g. Rout et al., 1993; Brunner et al., 1999; Schulz et al., 2005; Lindner et al., 2006; Cassidy et al., 2007; Lopez Loera et al., 2008; Mrlina et al., 2009; Skacelova et al., 2010; Blaikie et al., 2012; Barde-Cabusson et al., 2013), however the link between the geophysical interpretations, observations of surface deposits and the eruptive histories of the volcanoes could be improved upon. The results of geophysical studies of four different maar volcanoes from the Newer Volcanics Province of South-eastern Australia are examined in this paper.
A new Volcanic managEment Risk Database desIgn (VERDI): Application to El Hierro Island (Canary Islands)
2014, Journal of Volcanology and Geothermal ResearchCitation Excerpt :This type of geophysical data is useful in susceptibility analyses and in both short- and long-term hazard evaluations. In addition, it is useful for studying dispersed volcanic fields and their relation to local tectonics (Barde-Cabusson et al., 2014) and can thus facilitate a complete analysis of the probability of future activity in monogenetic fields and improve understanding of the internal structure of composite volcanoes (Rout et al., 1993; Blakely et al., 1997; Connor et al., 2000; Kiyosugi et al., 2010). Moreover, in both short- and long-term hazard assessments the monitoring and interpretation of geophysical parameters such as temporal gravity changes, seismicity and ground deformation can benefit from integration with structural geophysical data.
A model for calculating eruptive volumes for monogenetic volcanoes - Implication for the Quaternary Auckland Volcanic Field, New Zealand
2013, Journal of Volcanology and Geothermal ResearchThree-dimensional potential field modelling of a multi-vent maar-diatreme - The Lake Coragulac maar, Newer Volcanics Province, south-eastern Australia
2012, Journal of Volcanology and Geothermal Research
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Present address: Department of Geology, The University of Western Australia, Nedlands, Perth, W.A. 6009, Australia.