Temporal Evolution of a High-K Andesitic Magmatic System: Taranaki Volcano, New Zealand
نویسندگان
چکیده
منابع مشابه
Evolution of a Submarine Magmatic-Hydrothermal System: Brothers Volcano, Southern Kermadec Arc, New Zealand
Brothers volcano, which is part of the active Kermadec arc, northeast of New Zealand, forms an elongate edifice 13 km long by 8 km across that strikes northwest-southeast. The volcano has a caldera with a basal diameter of ~3 km and a floor at 1,850 m below sea level, surrounded by 290to 530-m-high walls. A volcanic cone of dacite rises 350 m from the caldera floor and partially coalesces with ...
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Pollen and charcoal analyses of sediments from northern coastal Taranaki, New Zealand, show that Maori settlement impacts on the vegetation began with the burning of tall coastal forest in the mid-17th century. Forest was replaced with a fern-shrubland, and small wetlands expanded with changing hydrological conditions. This forest clearance was much later than in most regions of the country, wh...
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a r t i c l e i n f o The silicic dome complex of Santiaguito, Guatemala, has exhibited continuous extrusive activity for 90 years. Despite its longevity, remarkably little is known about the magmatic plumbing system beneath Santiaguito. Here, we use petrological analyses of lava samples to define this plumbing system, from storage in the lower to mid-crust through to extrusion onto the surface...
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The measurement and analysis of seismicity in active volcanic areas is the main tool used in volcanic hazard mitigation. However, seismic monitoring technologies have met with only mixed success in forecasting eruptive episodes. This arises because, although our understanding of the spatio-temporal processes generating the observed seismic signals has increased substantially with the wide scale...
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ژورنال
عنوان ژورنال: Journal of Petrology
سال: 2011
ISSN: 1460-2415,0022-3530
DOI: 10.1093/petrology/egr064