Добірка наукової літератури з теми "Rabaul Caldera, magma mixing"
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Статті в журналах з теми "Rabaul Caldera, magma mixing"
Ronchin, Erika, Timothy Masterlark, John Dawson, Steve Saunders, and Joan Martì Molist. "Imaging the complex geometry of a magma reservoir using FEM-based linear inverse modeling of InSAR data: application to Rabaul Caldera, Papua New Guinea." Geophysical Journal International 209, no. 3 (March 24, 2017): 1746–60. http://dx.doi.org/10.1093/gji/ggx119.
Повний текст джерелаNakagawa, Mitsuhiro, and Ken-ichiro Aoki. "Petrology of Moriyoshi volcano - Magma mixing event after caldera collapse." Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists 80, no. 4 (1985): 136–54. http://dx.doi.org/10.2465/ganko1941.80.136.
Повний текст джерелаRobin, Claude, and Alain Potrel. "Multi-stage magma mixing in the pre-caldera series of Fuego de Colima volcano." Geofísica Internacional 32, no. 4 (October 1, 1993): 605–15. http://dx.doi.org/10.22201/igeof.00167169p.1993.32.4.606.
Повний текст джерелаClarke, L. B., and M. J. Le Bas. "Magma mixing and metasomatic reaction in silicate-carbonate liquids at the Kruidfontein carbonatitic volcanic complex, Transvaal." Mineralogical Magazine 54, no. 374 (March 1990): 45–56. http://dx.doi.org/10.1180/minmag.1990.054.374.04.
Повний текст джерелаHübner, Marcel, Christoph Breitkreuz, Alexander Repstock, Bernhard Schulz, Anna Pietranik, Manuel Lapp, and Franziska Heuer. "Evolution of the Lower Permian Rochlitz volcanic system, Eastern Germany: reconstruction of an intra-continental supereruption." International Journal of Earth Sciences 110, no. 6 (July 14, 2021): 1995–2020. http://dx.doi.org/10.1007/s00531-021-02053-5.
Повний текст джерелаBouvet de Maisonneuve, C., F. Costa, H. Patia, and C. Huber. "Mafic magma replenishment, unrest and eruption in a caldera setting: insights from the 2006 eruption of Rabaul (Papua New Guinea)." Geological Society, London, Special Publications 422, no. 1 (2015): 17–39. http://dx.doi.org/10.1144/sp422.2.
Повний текст джерелаLipman, Peter W. "Evolution of silicic magma in the upper crust: the mid-Tertiary Latir volcanic field and its cogenetic granitic batholith, northern New Mexico, U.S.A." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 79, no. 2-3 (1988): 265–88. http://dx.doi.org/10.1017/s0263593300014279.
Повний текст джерелаDeering, Chad D., Thomas A. Vogel, Lina C. Patino, and Guillermo E. Alvarado. "Origin of distinct silicic magma types from the Guachipelín Caldera, NW Costa Rica: Evidence for magma mixing and protracted subvolcanic residence." Journal of Volcanology and Geothermal Research 165, no. 3-4 (September 2007): 103–26. http://dx.doi.org/10.1016/j.jvolgeores.2007.05.004.
Повний текст джерелаTakashima, Shino, Yutaka Wada, and Hironao Shinjoe. "Miyanotani composite dike in central Kii Peninsula, southwest Japan: Implications for magma mixing and caldera volcanism." Journal of the Geological Society of Japan 116, no. 9 (2010): 496–509. http://dx.doi.org/10.5575/geosoc.116.496.
Повний текст джерелаMacdonald, R., B. Bagiński, B. G. J. Upton, P. Dzierżanowski, W. Marshall-Roberts, and M. Prieto. "The Palaeogene Eskdalemuir dyke, Scotland: long-distance lateral transport of rhyolitic magma in a mixed-magma intrusion." Mineralogical Magazine 73, no. 2 (April 2009): 285–300. http://dx.doi.org/10.1180/minmag.2009.073.2.285.
Повний текст джерелаДисертації з теми "Rabaul Caldera, magma mixing"
Streffon, Jenna C. "Magma Mixing and Dome Formation: Dacite of East Pass Creek, Colorado." Bowling Green State University / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1556705059361473.
Повний текст джерелаPatia, Herman. "Petrology and geochemistry of the recent eruption history at Rabaul Caldera, Papua New Guinea : implications for magmatic processes and recurring volcanic activity." Master's thesis, 2004. http://hdl.handle.net/1885/7345.
Повний текст джерелаThe Australian overseas Aid Agency (AusAID), in the form of an AusAID Scholarship Award. The ACT branch of the Geological Society for funding my participation at the 16th Australian Geological Convention held in Adelaide in July 2002. The Department of Mining for paying for air tickets and allowance for my family.
Sosa, Ceballos Giovanni 1975. "Evolution of Plinian magmas from Popocatépetl Volcano, México." Thesis, 2011. http://hdl.handle.net/2152/26905.
Повний текст джерелаtext
Ζούζιας, Δημήτριος. "Αειφόρος ανάπτυξη του ηφαιστείου της Νισύρου και νέα ηφαιστειολογικά χαρακτηριστικά στοιχεία της ευρύτερης περιοχής και με την συμβολή της τηλεπισκόπησης". Thesis, 2011. http://hdl.handle.net/10889/5673.
Повний текст джерелаThe Kos - Nisyros study area is located at the easternmost edge of the active Quaternary volcanic arc of the southern Aegean Sea and includes the islands of Kos and Nisyros and the islets of Gyali, Strongyli, Pachia and Pyrgoussa. The volcanic activity of Kos island is characterized by Upper – Miocene ignimbrite deposits and Pliocene - Pleistocene volcanic products such as volcanic domes, the Kefalos pyroclastic sequence of hydromagmatic tuffs and the large-scale pyroclastic formation Kos Plateau Tuff (KPT) deposits which is also found on the Kalymnos, Pserimos and Tilos islands. Nisyros is a calcalkaline stratovolcano which consists of Pliocene volcanic products such as andesite and basaltic andesite lavas that are overlain by pyroclastic deposits, lava flows and lava domes of dacitic – rhyodacitic composition. The islets of Gyali, Strongyli, Pachia and Pyrgoussa represent Pliocene lava domes of rhyolitic (Gyali), andesitic (Strogyli) and dacitic composition (Pachia and Pyrgoussa) On these domes, pyroclastic deposits of the Upper Pumice unit of Gyali (in Strogyli) and pyroclastic deposits of the Kos Plateau Tuff (KPT) and Panayia Kyra formation (in Pachia and Pyrgoussa) have been identified. In this thesis, the volcanic products of the Kos-Nisyros area are examined using mineral chemistry, geochemical and petrographical methods, while volcanic structures and morphological features are identified and mapped using remote sensing techniques. The aim of this thesis is to understand the volcanic evolution of the study area, by drawing conclusions regarding the consanguineous relationship of the magmatic products, magma mixing phenomena and the magma chamber system of the area, as well as, the surface expression of this magma chamber system in the form of caldera structures. For this purpose, in this thesis, it is investigated the consanguineous relationship of the Kos Tuff (Kos Plateau Tuff) found on Kos, Tilos and Kalymnos islands, as well as, the geochemical differentiation of the most violent and explosive ignimbrite units D and E of the Kos Tuff, confirming the stratigraphic correlation of these deposits as it was previously presented by physical volcanology data. The petrochemical study of the Kos - Nisyros area as a single "volcanic complex" reveals that the volcanism of the study area is divided into a Miocene and a Pliocene – Pleistocene activity. The Miocene activity is characterized by magmatic and volcanic products such as the monzonite of Kos and the Miocene ignimbrites of Kos and the Pliocene – Pleistocene volcanic activity consists of volcanic products such as lava domes and pyroclastic deposits from Kos, Gyali and Nisyros volcanoes where it is revealed the consanguineous magmatic relationship of these Pliocene – Pleistocene products. Using “Nomarski” interferometry method it is revealed that magma mixing/mingling phenomena are unquestionable for the magma chamber system of Nisyros and provide evidence that these phenomena were active throughout the volcanic evolution of Nisyros volcano. Field observations and remote sensing methods revealed caldera structures in the Kos - Nisyros area which are identified and classified according to new perceptions regarding the volcanic evolution. The volcanic structures of Nisyros volcano are examined using remote sensing methods such as satellite image and digital elevation models interpretation, as well as, the geomorphometric analysis of the Nisyros terrain in combination with geomorphotectonic features of the volcano as presented by other researchers and new perceptions on the volcanic evolution. It is also presented a model of proto-caldera, caldera and post-caldera evolution of Nisyros volcano based on new perceptions on the volcanic evolution in relation to the stratigraphic evolution. Finally, it is studied the subvolcanic magma chamber system of the Kos - Nisyros area, as well as, mixing phenomena in the volcano of Nisyros using the “Nomarski” interferometry method and the distribution of major, trace and rare earth elements revealing the consanguineous nature of these volcanic centers by providing the widest volcanic area of Kos - Nisyros as a major volcanic center characterized by a complex caldera system. Sustainable development of Nisyros volcano represents a management tool which combines the volcanic evolution with the environmental preservation and can promote volcanic regions as geotopes. The investigation of the present conditions of the island reveals, despite the fact that Nisyros is characterized by a strong environmental, energy, social, cultural and economic potential, it remains undeveloped and unexploited due to lack of an integrated sustainable development management plan, based on which, decisions should be equal, equivalent simultaneously and in harmony. Based on the study of the Nisyros water resources, the energy potential from renewable energy sources, the management of natural and urban environment of the volcano of Nisyros and the study of the positive and/or negative effects of the mining industry in Gyali volcanic islet it is proposed an integrated sustainable development according to the views and the perspectives of the local community. From this intergraded plan are generated recommendations for an integrated management of the volcano of Nisyros which satisfy equal, equivalent, simultaneously and in harmony the principles of sustainable development aiming to refocus the local economy, the management of natural and urban environment and the social development.