Relevant bibliographies by topics / Volcanological research

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters

Academic literature on the topic 'Volcanological research'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 January 2023

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Journal articles on the topic "Volcanological research"

1

Ueda, Hideki, Taishi Yamada, Takahiro Miwa, Masashi Nagai, and Takanori Matsuzawa. "Development of a Data Sharing System for Japan Volcanological Data Network." Journal of Disaster Research 14, no. 4 (June 1, 2019): 571–79. http://dx.doi.org/10.20965/jdr.2019.p0571.

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In Japan, a number of universities, research institutes, and administrative organizations continue to conduct observations on volcanoes according to their respective roles. They also promote the distribution and sharing of observation data and have collaborated with each other. Japan Volcanological Data Network (JVDN) is a framework that strengthens this cooperation, promotes volcano research, and contributes to volcanic disaster mitigation. In this paper, we report the overview, progress, tasks, and future prospects of the system being developed for JVDN that was initiated in 2016. The observational data collected from each organization is stored in a database and shared using visualization tools to promote collaborative research, (e.g., multi-disciplinary research for eruption prediction) and cooperation between organizations. Furthermore, this database will contribute to volcanic disaster mitigation measures through collaboration between the volcano research community and administrative organizations responsible for volcanic crisis management. Adaptation to the standards of the international WOVOdat database will also promote cooperation with research institutes worldwide.
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Wijaya, M. E. J., and L. D. Setijadji. "A Preliminary Volcanological Study of North Eastern Kaba Volcano, Bengkulu Province, Indonesia." IOP Conference Series: Earth and Environmental Science 1071, no. 1 (August 1, 2022): 012018. http://dx.doi.org/10.1088/1755-1315/1071/1/012018.

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Abstract Mount Kaba is one of the active volcanoes located in the eastern part of Bengkulu Province. This research was conducted in Gunung Kaba Complex because the distribution location of the last eruption product is close to some monogenetic volcano and residential area. This is interesting to study considering because can be a potential threat of disaster. The results of this study are expected to support providing an overview of the potential threat of volcanic disasters in the Mount Kaba Complex. The research methods used include geomorphological, stratigraphic, petrographic, and geochemical analyses. The geomorphological unit of Mount Kaba consists of 6 units. The types of volcanic rocks in the research area are dominated by lava and pyroclastic rocks. Based on the petrographic analysis of 10 samples, the names of the rocks in the research area are basalt scoria, basalt, and andesite. Based on the geochemical analysis of 8 samples, it is known that silica content in the rocks ranging from 44.40925 - 63.2993 %. Based on the AFM diagram, all samples are included in the tholeiitic series. Based on the TAS (Total Alkali Silica) diagram, it is known that the igneous rocks of the study area consist of andesite, basalt, tephrite, and trachyandesite.
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Pascual, Emilio, Teodosio Donaire, Manuel Toscano, Gloria Macías, Christian Pin, and Michael Hamilton. "Geochemical and Volcanological Criteria in Assessing the Links between Volcanism and VMS Deposits: A Case on the Iberian Pyrite Belt, Spain." Minerals 11, no. 8 (July 30, 2021): 826. http://dx.doi.org/10.3390/min11080826.

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VMS deposits in the Iberian Pyrite Belt (IPB), Spain and Portugal, constitute the largest accumulation of these deposits on Earth. Although several factors account for their genetic interpretation, a link between volcanism and mineralization is generally accepted. In many VMS districts, research is focused on the geochemical discrimination between barren and fertile volcanic rocks, these latter being a proxy of VMS mineralization. Additionally, the volcanological study of igneous successions sheds light on the environment at which volcanic rocks were emplaced, showing an emplacement depth consistent with that required for VMS formation. We describe a case on the El Almendro–Villanueva de los Castillejos (EAVC) succession, Spanish IPB, where abundant felsic volcanic rocks occur. According to the available evidence, their geochemical features, εNd signature and U–Pb dates suggest a possible link to VMS deposits. However, (paleo)volcanological evidence here indicates pyroclastic emplacement in a shallow water environment. We infer that such a shallow environment precluded VMS generation, a conclusion that is consistent with the absence of massive deposits all along this area. We also show that this interpretation lends additional support to previous models of the whole IPB, suggesting that compartmentalization of the belt had a major role in determining the sites of VMS deposition.
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Bondarenko, V. I., and V. A. Rashidov. "Underwater gas-hydrothermal activity within the Kuril island arc." Geosystems of Transition Zones 5, no. 1 (2021): 4–13. http://dx.doi.org/10.30730/gtrz.2021.5.1.004-013.

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The Kuril island arc is an important element of the Pacific transition zone, within which such modern geological processes as underwater gas-hydrothermal activity occur. The study of underwater gas-hydrothermal activity, which affects the natural environment and all life activities, has not only fundamental but also a great practical importance. The article provides a review of research studies into the underwater gas-hydrothermal activity of the Kuril island arc. New information on the manifestations of underwater gas-hydrothermal activity within this zone obtained as a result of processing, revision and analysis of materials of complex volcanological shipboard studies at the Volcanolog research vessel (1981–1991) is presented.
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Braz Machado, F., E. Reis Viana Rocha-Júnior, L. Soares Marques, and A. J. Ranalli Nardy. "Volcanological aspects of the northwest region of Paraná continental flood basalts (Brazil)." Solid Earth 6, no. 1 (February 19, 2015): 227–41. http://dx.doi.org/10.5194/se-6-227-2015.

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Abstract. There has been little research on volcanological aspects of Paraná continental flood basalts (PCFBs), and all investigations have mainly been concentrated on the internal portions of the lava flows. Thus, this study describes for the first time morphological aspects of lava flows and structural characteristics caused by lava–sediment interaction in the northwestern PCFB province (NW-PCFB). Early Cretaceous (134 to 132 Ma) tholeiitic rocks of the PCFB were emplaced on a large intracratonic Paleozoic sedimentary basin (Paraná Basin), mainly covering dry eolian sandstones (Botucatu Formation). As this sedimentary unit is overlain by the basic lava flows of the PCFB, the interaction of lavas and unconsolidated sediments resulted in the generation of fluidal peperites. This aspect is significant because it shows that restricted wet environments should have existed in the Botucatu desert. The peperite zones of the NW-PCFB are associated with compound pahoehoe-type (P-type) flows and are always related to the first volcanic pulses. These flows have dispersed vesicles and sand-filled cracks in their base and top borders, as well as the presence of interlayered sandstones with irregular contacts and varied thicknesses. It is remarkable that, to the best of current knowledge, only in this area of the whole PCFB did the volcanic activity start with low-Ti basalt flows of Ribeira type (TiO2 < 2.3 wt%), which are scarce in the province.
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Kavanagh, Janine L., Samantha L. Engwell, and Simon A. Martin. "A review of laboratory and numerical modelling in volcanology." Solid Earth 9, no. 2 (April 27, 2018): 531–71. http://dx.doi.org/10.5194/se-9-531-2018.

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Abstract. Modelling has been used in the study of volcanic systems for more than 100 years, building upon the approach first applied by Sir James Hall in 1815. Informed by observations of volcanological phenomena in nature, including eye-witness accounts of eruptions, geophysical or geodetic monitoring of active volcanoes, and geological analysis of ancient deposits, laboratory and numerical models have been used to describe and quantify volcanic and magmatic processes that span orders of magnitudes of time and space. We review the use of laboratory and numerical modelling in volcanological research, focussing on sub-surface and eruptive processes including the accretion and evolution of magma chambers, the propagation of sheet intrusions, the development of volcanic flows (lava flows, pyroclastic density currents, and lahars), volcanic plume formation, and ash dispersal. When first introduced into volcanology, laboratory experiments and numerical simulations marked a transition in approach from broadly qualitative to increasingly quantitative research. These methods are now widely used in volcanology to describe the physical and chemical behaviours that govern volcanic and magmatic systems. Creating simplified models of highly dynamical systems enables volcanologists to simulate and potentially predict the nature and impact of future eruptions. These tools have provided significant insights into many aspects of the volcanic plumbing system and eruptive processes. The largest scientific advances in volcanology have come from a multidisciplinary approach, applying developments in diverse fields such as engineering and computer science to study magmatic and volcanic phenomena. A global effort in the integration of laboratory and numerical volcano modelling is now required to tackle key problems in volcanology and points towards the importance of benchmarking exercises and the need for protocols to be developed so that models are routinely tested against real world data.
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Tsutsui, Tomoki, Yoshiharu Hirayama, Toshiharu Ikeda, Keiji Takeuchi, and Hiroshi Ando. "Feasibility Study on a Multi-Channeled Seismometer System with Phase-Shifted Optical Interferometry for Volcanological Observations." Journal of Disaster Research 14, no. 4 (June 1, 2019): 592–603. http://dx.doi.org/10.20965/jdr.2019.p0592.

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A new Phase-Shifted Optical Interferometry seismometer system was tested in terms of its feasibility for multi-channeled volcanological observations in two volcanos in Japan. The system is capable of both sensing ground motions and transferring its signals through optical means. The prototype of this system comprises three optical-wired stations and optical components, and was deployed in Sakurajima Volcano in 2016 and in Asama Volcano in 2017. The system successfully operated for 134 days in total and provided seismograms that are in good agreement with those obtained using conventional systems. Several obstacles for putting this system to practical use that need to be solved were found through tests. Their solutions will be explored in subsequent research.
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Druitt, Timothy H., Floyd W. McCoy, and Georges E. Vougioukalakis. "The Late Bronze Age Eruption of Santorini Volcano and Its Impact on the Ancient Mediterranean World." Elements 15, no. 3 (June 1, 2019): 185–90. http://dx.doi.org/10.2138/gselements.15.3.185.

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The Late Bronze Age eruption of Santorini occurred 110 km north of Minoan Crete (Greece). Having discharged between 48 and 86 km3 of magma and rock debris, the eruption ranks as one of the largest of the last 10,000 years. On Santorini, it buried the affluent trading port of Akrotiri. Modern volcanological research has reconstructed the eruption and its regional impacts in detail, while fifty years of archaeological excavations have unraveled the events experienced by the inhabitants of Akrotiri during the months that led up to the eruption. Findings do not favour a direct relationship between the eruption and the decline of the Minoan civilization, although tsunamis and atmospheric effects may have weakened Cretan society through impacts on shipping, trade and agriculture.
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Stefano Branca, Daniele Musumeci, and Luigi Ingaliso. "The significance of the 1971 flank eruption of Etna from volcanological and historic viewpoints." Annals of Geophysics 64, no. 5 (December 13, 2021): VO543. http://dx.doi.org/10.4401/ag-8669.

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The 1971 eruption represents a benchmark in the recent history of Etna volcano. From a volcanological point of view, this eruption was characterised by complex intrusive dynamics associated with significant ground deformation that induced the activation of the Moscarello seismogenic fault and the formation of a new summit crater: the Southeast Crater. At the same time, the 1971 event marks an important change in the eruptive style and composition of the magma towards products richer in K. It is no coincidence that, over the next fifty years, there would be an increase in the frequency of summit and flank eruptions and associated output rate. From an historical viewpoint, the eruptive event of 1971 was the first important flank eruption studied by the International Institute of Volcanology: the analysis of the scientific articles on this activity reveals a greater multidisciplinary content in the descriptions and explanations of volcanic activity. Particularly important were the collaborations of British and French research groups that, together with their Italian colleagues, succeeded in giving a complete picture of the eruption and describing the state of knowledge on the Sicilian volcano. The multidisciplinary methodology used to study this eruption is still valid today.
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Shakirova, Alexandra, Pavel Firstov, and Mikhail Lemzikov. "One of the possible mechanisms for generating the seismic mode “drumbeats” when moving the Kizimen Volcano viscous lava flow along the slope in 2011-2012." Russian Journal of Seismology 2, no. 3 (September 30, 2020): 43–56. http://dx.doi.org/10.35540/2686-7907.2020.3.04.

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"Drumbeats" is an unusual seismic mode consisting of volcanic micro-earthquakes with monotonous waveforms (multiplets) that are recorded from tens of minutes to months. Due to the quasi-regularity of the occurrence of earthquakes, the mode was called "drumbeats". The "drumbeats" mode is registered when individual blocks are squeezed out on the extrusive domes of andesite and dacite volcanoes of the world and occurs at stable equilibrium states in the channel-magma system during an eruption. For the first time in the world practice of volcanological research, the "drumbeats" mode was registered, accompanying the movement of a viscous lava flow with a volume of 0.3 km3 of the Kizimen volcano eruption in 2010-2013. The paper considers kinematic and dynamic parameters of micro-earthquakes of the "drumbeats" mode, their mechanisms, and offers a phenomenological model for generating the "drumbeats" mode that occurs when a lava flow moves along the slope of the Kizimen volcano.
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Dissertations / Theses on the topic "Volcanological research"

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McClintock, Murray, and n/a. "Physical volcanology of the Sterkspruit flood basalt crater complex, South Africa." University of Otago. Department of Geology, 2007. http://adt.otago.ac.nz./public/adt-NZDU20070601.161342.

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Volcanism associated with the onset of Karoo flood basalt eruptions (c. 180 Ma) at Sterkspruit, South Africa, began with emplacement of thin lava flows before abruptly switching to phreatomagmatic and magmatic activity that formed a nest of craters, spatter and tuff rings and cones that collectively comprise a crater complex >40 km� filled by 9-18 km� of volcaniclastic debris. Phreatomagmatic activity driven by interaction of Karoo magma with groundwater hosted in country rock and crater-filling debris quarried broad, mainly shallow craters (hundreds of metres, but not kilometers deep) into wall-rock. Closely spaced individual vents, the consequence of magma emplaced over a broad area through a network of feeder dikes and stocks, were active at the same time or over short periods of time. Highly ephemeral access of external water to vents drove repeated and reversible switches between explosive to effusive magmatic and explosive phreatomagmatic activity, resulting in vents and craters that grew laterally and vertically into adjacent ones through quarrying and vent migration. Deposits within the Sterkspruit crater complex are dominated by 7-15 km� of massive, unsorted polymict lapilli tuff and tuff breccia juxtaposed with localised fountain-fed lava and strombolian spatter deposits. Transport within the complex was dominated by jets and fountains of volcaniclastic debris and by mass movement. Country-rock breccias indicate that craters grew via a combination of mechanical fragmentation, granulation and mass-movement of 7-12 km� of wall-rock, adding mass and previously locked-up pore-water to the volcanic system. Ash and lapilli, the deposits of plumes 5-15 km high, form a 50-110 m-thick ejecta blanket mantling Clarens Formation country rock that thins gradually away from the crater-complex margins. Explosive volcanism was succeeded by brief fluvial and eolian reworking of volcaniclastic debris and formation of a shallow crater lake 12 km� in extent, and then by voluminous effusion of flood basalt that inundated the Sterkspruit crater complex with lava. Flood basalt magmas involved in Sterkspruit eruptions were chemically heterogenous. This study documents the rapid (perhaps simultaneous) eruption of multiple, chemically distinct basaltic magmas, which cannot be simply related to one another, from one vent site, and possibly many others, within the Sterkspruit crater complex. Five distinct magma types were involved in eruptions at Sterkspruit, indicating that in the early stages of flood basalt eruption (i) magma batches may be small and not simply related to one another, (ii) heterogeneities in the magma source region may be close to each other in time and space, and (iii) eruptions of chemically distinct magmas may take place over short intervals of space and time without significant hybridisation. Formation of the Sterkspruit Complex, and many others like it in South Africa, confirms that the opening phases of Karoo flood basalt volcanism were explosive, and that the volume of the products of explosive volcanism may have important implications for climate change and landscape development associated with the emplacement of large igneous provinces.
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Lafrance, Benoît. "Reconstruction d'un environnement de sulfures massifs volcanogènes déformé : exemple archéen de Normétal, Abitibi /." Thèse, Chicoutimi : [Montréal : Université du Québec à Chicoutimi ; Université du Québec à Montréal], 2003. http://theses.uqac.ca.

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Thèse (D.Ress.Min.) -- Université du Québec à Chicoutimi, programme extensionné à l'Université du Québec à Montréal, 2003.
Bibliogr.: f. 267-278. Document électronique également accessible en format PDF. CaQCU
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Steiner, Arron Richard. "Field Geology and Petrologic Investigation of the Strawberry Volcanics, Northeast Oregon." PDXScholar, 2016. http://pdxscholar.library.pdx.edu/open_access_etds/2712.

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The Strawberry Volcanics of Northeast Oregon are a group of geochemically related lavas with a diverse chemical range (basalt to rhyolite) that erupted between 16.2 and 12.5 Ma and co-erupted with the large, (~200,000 km3) Middle Miocene tholeiitic lavas of the Columbia River Basalt Group (CRBG), which erupted near and geographically surround the Strawberry Volcanics. The rhyolitic lavas of the Strawberry Volcanics produced the oldest 40Ar/39Ar ages measured in this study with ages ranging from 16.2 Ma to 14.6 Ma, and have an estimated total erupted volume of 100 km3. The mafic and intermediate lavas of the Strawberry Volcanics include both tholeiitic and calc-alkaline compositions; calc-alkaline andesite is the dominant type by volume. 40Ar/39Ar ages of the mafic and intermediate lava flows range from 15.6 Ma to 12.5 Ma, and volume estimates of the intermediate lavas are approximately 1,100 km3. The magmas that gave rise to the Strawberry Volcanics traveled to the surface through numerous dikes, some of which have been exposed at the surface and supplied lava to fissure – style eruptions and/or shield volcanoes. Herein, we show that the Strawberry Volcanics are related to the CRBG in both time and space and share a chemical affinity, specifically to the Steens Basalt. Chemical similarities are observed in normalized trace element patterns, selected trace element ratios, and radiogenic isotopes. Comparison of the Strawberry Volcanic rhyolites to the other Middle Miocene rhyolites of eastern Oregon associated with the initiation of the Yellowstone – Snake River mantle plume reveals similar eruption ages, trace element compositions, including the rare earth elements (REEs), and "A-type" rhyolite characteristics. These data suggest that the Strawberry Volcanics are part of the regional volcanism (basalt to rhyolite) of the Columbia River Basalt Province. The petrogenesis of the Strawberry Volcanics can be explained as follows: 1) The tholeiitic, intermediate magmas were produced by fractional crystallization of mafic magmas, which have a commonality with the surrounding Columbia River Basalt Group; 2) The calc-alkaline magmas are a result of mixing between tholeiitic basalt, rhyolite, and crust. The arc-like signature of the calc-alkaline lavas (elevated large ion lithophiles) is a result of both the melting source region and the end-members with which the mafic magmas mixed/contaminated. Other authors have produced similar findings from within the Basin and Range/Oregon-Idaho graben and CRB province. The difference at the Strawberry Volcanics is that there is no need for a primitive calc-alkaline magma or extensive fractional crystallization to generate the calc-alkaline andesites. Alternatively, the calc-alkaline magmas of the Strawberry Volcanics were generated by a more primitive tholeiitic magma than erupted at the surface, which interacted with crustal melts and assimilated crustal lithologies from the complex zone of assimilated terranes that make up the basement of eastern Oregon.
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Barnie, Talfan Donald. "Estimating lava effusion rates from geostationary satellite thermal images : a novel time series analysis and linear inversion approach applied to the eruptions of Afar, Ethiopia, between 2007 and 2010." Thesis, University of Cambridge, 2015. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.708893.

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Piché, Mathieu. "La formation de Hauy à l'ouest de Chapais ; volcanisme sub-aérien en milieu fluviatile /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1985. http://theses.uqac.ca.

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Mémoire (M.Sc.A.Geologie)--Université du Québec à Chicoutimi, 1985.
Une carte pliée, en pochette. "Mémoire présenté en vue de l'obtention de la maîtrise en sciences appliquées en géologie" CaQCU CaQCU Document électronique également accessible en format PDF. CaQCU
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Meilleur, Dominique. "Distribution de la taille des cristaux (DTC) et géochimie des laves rhyolitiques de la chaîne volcanique Inyo, Long Valley, Californie /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2004. http://theses.uqac.ca.

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Landry, Jacques. "Volcanologie physique et sédimentologie du groupe volcanique de Piché et relations stratigraphiques avec les groupes sédimentaires encaissants de Pontiac et de Cadillac /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1991. http://theses.uqac.ca.

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Potvin, Robin. "Étude volcanologique du centre volcanique felsique du lac des Vents, région de Chibougamau /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1991. http://theses.uqac.ca.

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Griffin, Anna M. "Products and processes of cone-building eruptions from North Crater, Tongariro." 2007. http://adt.waikato.ac.nz/public/adt-uow20070219.150524/index.html.

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Books on the topic "Volcanological research"

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Iceland) George Walker Memorial Meeting (2006 Reykholt. Studies in volcanology: The legacy of George Walker. London: Geological Society, 2009.

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Shenzhen Shi (China). Di zhi ju and Shenzhen Shi di zhi xue hui, eds. Shenzhen Dapeng Bandao guo jia di zhi gong yuan gu huo shan di zhi yi ji diao cha yan jiu. Wuhan Shi: Zhongguo di zhi da xue chu ban she, 2010.

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Geological Survey (U.S.), ed. Monitoring active volcanoes. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Tilling, Robert I. Monitoring active volcanoes. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Branney, M. J. Pyroclastic density currents and the sedimentation of ignimbrites. London: Geological Society, 2002.

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1941-, Smith Alan L., ed. Volcanology of Saba and St. Eustatius, Northern Lesser Antilles. Amsterdam: Royal Netherlands Academy of Arts and Sciences, 2004.

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Ferrer, Anthony P. Pillars of Philippine geology: Prof. Arturo P. Alcaraz, 1916-2001 : a legacy of pioneering work in volcanology and geothermal energy development. Manila: PNOC-Energy Development Corp., 2002.

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Assembly, International Association of Volcanology and Chemistry of the Earth's Interior General. IAVCEI, Canberra 1993: Excursion guide : General Assembly, September 1993, Camberra, Australia : ancient volcanism & modern analogues. Canberra [A.C.T.]: Australian Geological Survey Organisation, 1993.

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Dzurisin, Daniel. Volcano deformation: Geodetic monitoring techniques. Berlin: Springer, 2007.

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Geissman, John William, M. H. Ort, and M. Porreca. The use of palaeomagnetism and rock magnetism to understand volcanic processes. London: The Geological Society, 2015.

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Book chapters on the topic "Volcanological research"

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Nemeth, Karoly. "An Overview of the Monogenetic Volcanic Fields of the Western Pannonian Basin: Their Field Characteristics and Outlook for Future Research from a Global Perspective." In Updates in Volcanology - A Comprehensive Approach to Volcanological Problems. InTech, 2012. http://dx.doi.org/10.5772/23219.

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Li, Boxin, Károly Németh, Julie Palmer, Alan Palmer, Jing Wu, Jonathan Procter, and Jiaqi Liu. "Basic Volcanic Elements of the Arxan-Chaihe Volcanic Field, Inner Mongolia, NE China." In Volcanoes - Updates in Volcanology [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.94134.

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The Arxan-Chaihe Volcanic Field, Inner Mongolia, NE China is a Pleistocene to Recent volcanic field still considered to be active. In this chapter we provide an update of current volcanological research conducted in the last four years to describe the volcanic architecture of the identified vents, their eruptive history and potential volcanic hazards. Here we provide an evidence-based summary of the most common volcanic eruption styles and types the field experienced in its evolution. The volcanic field is strongly controlled by older structural elements of the region. Hence most of the volcanoes of the field are fissure-controlled, fissure-aligned and erupted in Hawaiian to Strombolian-style creating lava spatter and scoria cone cone chains. One of the largest and most complex volcano of the field (Tongxin) experienced a violent phreatomagmatic explosive phase creating a maar in an intra-mountain basin, while the youngest known eruptions formed a triple vent set (Yanshan) that reached violent Strombolian phases and created an extensive ash and lapilli plains in the surrounding areas. This complex vent system also emitted voluminous lava flows that change the landscape by damming fluival networks, providing a volcanological paradise for the recently established Arxan UNESCO GLobal Geopark.
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