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Silicic calderas and volcanic centres in Coromandel volcanic zone






Geological Society of New Zealand Miscellaneous Publication 116A: 22

Silicic calderas and volcanic centres in Coromandel volcanic zone


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Accession: 020017920



Related references

Briggs R.M.; Houghton B.F.; McWilliams M.; Wilson C.J.N., 2005: Super 40 Ar- super 39 Ar ages of silicic volcanic rocks in the Tauranga-Kaimai area, New Zealand; dating the transition between volcanism in the Coromandel Arc and the Taupo volcanic zone. Subduction-related volcanism in the northern part of the North Island of New Zealand shifted abruptly during the late Pliocene. This study focuses on the transition, in time and space, from the NNW-oriented Miocene-Pliocene Coromandel Volcanic Zon...

Blattner Peter; H.R.i Zhong; Graham Ian J.; Houston Eleftheriadis Caroline, 1996: Temperature and isotopic evolution of silicic magmas, Taupo volcanic zone and Coromandel, New Zealand. A new set of oxygen and strontium isotope data on rhyolitic lavas and ignimbrites of the Taupo Volcanic Zone (TVZ) and the Coromandel Peninsula provides new limits for petrogenetic models. For oxygen isotopes, the rock matrix is frequently altered...

Houghton Bruce F.; Wilson C.J.N.; McWilliams M.; Lanphere M.A.; Pringle Malcolm S., 1992: Volcanic and structural evolution of a large silicic volcanic system; the Taupo volcanic zone, New Zealand. Eos, Transactions, American Geophysical Union 73(14, suppl

Browne P.R.L.; Wood C.P., 1987: Geological significance of recent geothermal drilling in volcanic centers and calderas of the Taupo volcanic zone. International Union of Geodesy and Geophysics, General Assembly 19, Vol

Houghton B.F.; Wilson C.J.N.; McWilliams M.O.; Pringle M.S.; Lanphere M.A., 1992: Caldera evolution of Taupo volcanic zone, New Zealand; a large volume silicic volcanic system. International Geological Congress, Abstracts Congres Geologique Internationale, Resumes: ages 480. 1992.

Rose W.I.J.; Bornhorst T.J.; Wunderman R.L., 1981: Quaternary calderas of Guatemala and El Salvador and silicic volcanic rocks. Abstracts with Programs - Geological Society of America 13(7): 540-541

Hughes Gwyneth R.; Mahood Gail A., 2008: Tectonic controls on the nature of large silicic calderas in volcanic arcs. Silicic magma bodies stabilize the continental margin by redistributing low-density material into the upper crust. We examined the tectonic traits of 91 young, arc-related, silicic calderas to test previous assertions that the nature of voluminous...

Malengreau B.; Skinner D.N.B.; Bromley C.J.; Black P., 2000: Geophysical characterisation of large silicic volcanic structures in the Coromandel Peninsula, New Zealand. Previous stratigraphic and tectonic studies of Coromandel Peninsula, New Zealand, have defined regionally significant structures, including calderas, of Miocene age. A new gravity map of the area reveals significant details not seen in the earlier...

Anonymous, 2008: Reconstructing the Quaternary evolution of the world's most active silicic volcanic system: insights from an ˆ¼1.65 Ma deep ocean tephra record sourced from Taupo Volcanic Zone, New Zealand

Allan, A.S.R.; Baker, J.A.; Carter, L.; Wysoczanksi, R.J., 2008: Reconstructing the Quaternary evolution of the worlds most active silicic volcanic system; insights from an approximately 165 Ma deep ocean tephra record sourced from Taupo volcanic zone, New; Zealand. The Taupo Volcanic Zone (TVZ), central North Island, New Zealand, is the most frequently active Quaternary rhyolitic system in the world. Silicic tephras recovered from Ocean Drilling Programme Site 1123 (41 degrees 47.16'S, 171 degrees 29.94...