Relevant bibliographies by topics / Volcanic

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Volcanic'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 July 2025

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Journal articles on the topic "Volcanic"

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Ludden, John, Claude Hubert, and Clement Gariépy. "The tectonic evolution of the Abitibi greenstone belt of Canada." Geological Magazine 123, no. 2 (1986): 153–66. http://dx.doi.org/10.1017/s0016756800029800.

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AbstractBased on structural, geochemical, sedimentological and geochronological studies, we have formulated a model for the evolution of the late Archaean Abitibi greenstone belt of the Superior Province of Canada. The southern volcanic zone (SVZ) of the belt is dominated by komatiitic to tholeiitic volcanic plateaux and large, bimodal, mafic-felsic volcanic centres. These volcanic rocks were erupted between approximately 2710 Ma and 2700 Ma in a series of rift basins formed as a result of wrench-fault tectonics.The SVZ superimposes an older volcanic terrane which is characterized in the north
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Yanev, Yotzo, Vlastimil Konečný, Alexandra Harkovska, Sergiu Peltz, and Pál Gyarmati. "Petrochemical characterisation of the Late Alpine orogenic acid volcanism of the Carpathian-Balkan area." Geologica Balcanica 25, no. 1 (1995): 3–12. http://dx.doi.org/10.52321/geolbalc.25.1.3.

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Late Apine orogenic volcanism appears immediately after the main phase of folding and thrusting in the Carpathian-Balkan area. The age of the volcainic manifestations is Priabonian-Oligocene (after Ilirian phase) in the Balkan segment and Miocene-Pliocene (after Savian phase) in the Carpathian segment, respectively. Most of the acid volcanics are formed by crustal melting, whereas a smaller part are differentiates of basaltic and intermediate magmas. The first one has higher SiO2 content than the second. K2O content increases from the North to the South: in the Carpatian segment the acid volca
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Smellie, John L., Kurt S. Panter, and Jenna Reindel. "Chapter 5.3a Mount Early and Sheridan Bluff: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 491–98. http://dx.doi.org/10.1144/m55-2018-61.

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AbstractTwo small monogenetic volcanoes are exposed at Mount Early and Sheridan Bluff, in the upper reaches of Scott Glacier. In addition, the presence of abundant fresh volcanic detritus in moraines at two other localities suggests further associated volcanism, now obscured by the modern Antarctic ice sheet. One of those occurrences has been attributed to a small subglacial volcano onlyc.200 km from South Pole, making it the southernmost volcano in the world. All of the volcanic outcrops in the Scott Glacier region are grouped in a newly defined Upper Scott Glacier Volcanic Field, which is pa
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Šimon, Ladislav, Viera Kollárová, and Monika Kováčiková. "Neogene volcanics of the Burda mountain range nearby Štúrovo, Slovakia." Mineralia Slovaca 55, no. 2 (2023): 117–32. http://dx.doi.org/10.56623/ms.2023.55.2.2.

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The Neogene volcanic products of the Burda mountain range nearby Štúrovo belong to Burda Formation. At the base of the Burda Formation a succession of epiclastic volcanic rocks and pyroclastic rocks of andesites has developed. In the central part of the formation, the volcanic products associated with the activity of submarine volcanism of the Badenian age developed. Submarine extrusive volcanic domes of andesites are typical. In the upper part of the Burda Formation, pyroclastic and epiclastic facies of andesites were formed. Deposits of pyroclastic flows and redeposited pyroclastics are char
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Sánchez, Florencia D., Jorge E. Romero, Paulo Pereira, and Manuel E. Schilling. "Geological heritage sites assessment in the northern flank of the Calbuco volcano (Southern Andes, Chile)." Andean Geology 51, no. 2 (2024): 357. http://dx.doi.org/10.5027/andgeov51n2-3651.

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Calbuco volcano (41.3° S, Southern Andes) ranks second in the Chilean volcanic risk ranking. The products of Calbuco’s last eruption (April 22-23, 2015) severely affected the surroundings of the volcano, particularly the Ensenada village (~1,500 inhab.), evidencing a growing need for effective volcanic risk management and mitigation. The geological study of volcanic deposits and landforms is a key step in reconstructing past volcanic eruptions and for the evaluation of volcanic hazards and associated risks. Additionally, well-preserved and easily accessible volcanic deposits can be considered
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Jundee, Patcharin Kosuwan, Yuenyong Panjasawatwong, Phisit Limtrakun, and Sirot Salyapongse. "Tectonic Implication of the Permo-Triassic Khao Yai Mafic Volcanic Rocks in Nakhon Nayok Province, Thailand: Evidence from Geochemistry and Rare Earth Elements (REEs)." Trends in Sciences 20, no. 7 (2023): 6582. http://dx.doi.org/10.48048/tis.2023.6582.

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The Permo-Triassic Khao Yai Volcanics in Nakhon Nayok Province, Thailand, is a part of the Loei-Phetchabun-Nakhon Nayok Volcanic Belt. The purpose of this study is to clarify the geochemistry and REEs characteristic of Khao Yai Volcanics that is useful for identifying the paleo-environment or tectonic setting eruption in this area. The least-altered, mafic volcanic rocks from the Permo-Triassic Khao Yai volcanics, are seriate-textured to porphyritic, with variable amounts of phenocrysts/microphenocrysts. The mineral compositions include plagioclase, clinopyroxene, orthopyroxene, olivine, minor
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Smellie, John L. "Chapter 3.2a Bransfield Strait and James Ross Island: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 227–84. http://dx.doi.org/10.1144/m55-2018-58.

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AbstractFollowing more than 25 years of exploration and research since the last regional appraisal, the number of known subaerially exposed volcanoes in the northern Antarctic Peninsula region has more than trebled, from less than 15 to more than 50, and that total must be increased at least three-fold if seamounts in Bransfield Strait are included. Several volcanoes remain unvisited and there are relatively few detailed studies. The region includes Deception Island, the most prolific active volcano in Antarctica, and Mount Haddington, the largest volcano in Antarctica. The tectonic environmen
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Ganelin, A. V., E. V. Vatrushkina, and M. V. Luchitskaya. "Geochemistry and geochronology of cretaceous volcanism of Chauna region, Central Chukotka." Геохимия 64, no. 1 (2019): 20–42. http://dx.doi.org/10.31857/s0016-752564120-42.

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New geochronological and geochemical data on the age and composition of Cretaceous volcanism of Palyavaam River basin (Central Chukotka, Chauna region) are presented. First complex is composed of rhyolites, ignimbrites and felsic tuffs of Chauna Group of Okhotsk-Chukotka volcanic belt (OCVB). Second complex is represented by volcanic rocks of latite-shoshonite series of Early Cretaceous age, distinguished as Etchikun’ Formation. Its origin is still debatable. Some researchers refer deposits of Etchikun’ Formation to magmatic stage before OCVB activity. Other authors include in Chauna Group com
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Tripathi, C. "Volcanism in Gondwanas." Journal of Palaeosciences 36 (December 31, 1987): 285–89. http://dx.doi.org/10.54991/jop.1987.1587.

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In India the Lower Permian event is marked by a major volcanic episode in the Himalayan belt and rift faulting in the Peninsula which gave rise to various Gondwana basins. The Lower Cretaceous major volcanic episode represented by the Rajmahal Trap represents the termination of Gondwana sedimentation. Lower Permian volcanism is represented by the Panjal Volcanics in Kashmir Basin and its equivalent, the Volcanics in Spiti-Zanskar Basin and Rotung Volcanics (Abor Volcanics) in Arunachal Pradesh. In Karakarom Basin of Ladakh, volcanism is associated with Changtash and Aqtash formations of Permia
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Yudiantoro, Dwi Fitri, Dyah Rini Ratnaningsih, Puji Pratiknyo, et al. "Magma Evolution of Ngebel Volcano, Ponorogo, East Java, Indonesia." Indonesian Journal on Geoscience 10, no. 1 (2023): 51–62. http://dx.doi.org/10.17014/ijog.10.1.51-62.

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The magma evolution of Ngebel Volcano, both temporally and spatially, is represented by the characteristics of its lava. Ngebel Volcano, located in East Java, is a Quaternary andesitic stratovolcano. This volcano is part of the Wilis Volcanic Complex. The volcanism stage of Ngebel Volcanic Complex can be divided into the Jeding with andesitic basalt (SiO2 49 - 59%), pyroxene andesite Kemlandingan (SiO2 49 - 59%), Manyutan with hornblende andesite (SiO2 49 - 59%), and Ngebel with dacite (SiO2: 49 - 59%). The variation of major elements combined with petrographic features such as plagioclase, py
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Dissertations / Theses on the topic "Volcanic"

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Purdy, David John. "Volcanic stratigraphy and origin of the Wallangarra Volcanics, Wandsworth volcanic group, northern NSW, Australia." Thesis, Queensland University of Technology, 2003.

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Smith, R. T. "Eruptive and depositional models for units 3 and 4 of the 1.85 ka Taupo eruption: Implications for the nature of large-scale 'wet' eruptions." Thesis, University of Canterbury. Geological Science, 1998. http://hdl.handle.net/10092/5928.

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Phreatomagmatic eruptions result from the explosive interaction between magma and some external source of water, and produce deposits which are usually distinctive in nature from those of magmatic eruptions. The widespread deposits of large-scale phreatomagmatic eruptions (usually termed Phreatoplinian) are poorly studied relative to their magmatic counterparts and, consequently, current models for large-scale phreatomagmatic volcanism remain speculative. The Hatepe ash and Rotongaio ash (units 3 and 4 of the 1.85 ka Taupo eruption) are two classical widespread phreatomagmatic fall deposits. T
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Bartolini, Stefania. "Volcanic hazard assessment in monogenetic volcanic fields." Doctoral thesis, Universitat de Barcelona, 2014. http://hdl.handle.net/10803/284845.

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One of the most important tasks of modern volcanology, which represents a significant socio-economic implication, is to conduct hazard assessment in active volcanic systems. These volcanological studies are aimed at hazard that allows to constructing hazard maps and simulating different eruptive scenarios, and are mainly addressed to contribute to territorial planning, definition of emergency plans or managing volcanic crisis. The impact of a natural event, as a volcanic eruption, can significantly affect human life, property, infrastructures, and the environment. Long periods of quiescence ar
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Wetie, Ngongang Ariane. "Seismic and Volcanic Hazard Analysis for Mount Cameroon Volcano." Diss., University of Pretoria, 2016. http://hdl.handle.net/2263/60871.

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Mount Cameroon is considered the only active volcano along a 1600 km long chain of volcanic complexes called the Cameroon Volcanic Line (CVL). It has erupted seven times during the last 100 years, the most recent was in May 2000. The approximately 500,000 inhabitants that live and work around the fertile flanks are exposed to impending threats from volcanic eruptions and earthquakes. In this thesis, a hazard assessment study that involves both statistical modelling of seismic hazard parameters and the evaluation of a future volcanic risk was undertaken on Mount Cameroon. The Gutenberg-Richter
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Hellwig, Bridget M. "The viscosity of dacitic liquids measured at conditions relevant to explosive arc volcanism determing the influence of temperature, silicate composition, and dissolved volatile content /." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4597.

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Thesis (M.S.)--University of Missouri-Columbia, 2006.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (February 7, 2007) Includes bibliographical references.
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Vallejo, Vargas Silvia Ximena. "Numerical models of volcanic flows for an estimation and delimitation of volcanic hazards, the case of Reventador volcano (Ecuador)." Thesis, Université Clermont Auvergne‎ (2017-2020), 2017. http://www.theses.fr/2017CLFAC100/document.

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Les coulées de laves sont les produits volcaniques les plus représentatifs des éruptions effusives. Elles sont formées quand le magma est extrudé et se répand à la surface de la Terre. Quand la lave arrive en surface, elle perd de la chaleur et refroidit. Le refroidissement affecte directement les propriétés rhéologiques de la lave, jusqu’à arrêter son écoulement. Les paramètres rhéologiques qui contrôlent la dynamique des coulées de laves sont la viscosité et le seuil de plasticité, qui dépendent eux-mêmes de la composition chimique, de la cristallinité et de la teneur en bulles. Il existe de
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Smith, Cassandra M. "Volcanic Electrification: A Multiparametric Case Study of Sakurajima Volcano, Japan." Scholar Commons, 2019. https://scholarcommons.usf.edu/etd/7950.

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Electrical activity at volcanoes has been recently recognized as a potential new remote sensing technique for plume-forming eruptions. Volcanic electrical activity takes place in the conduit and plume and therefore has the benefit of being a direct indicator of surface activity. This is unlike seismic signals, which indicate magma/gas movement underground, and infrasound signals, which indicate a surface explosion but not necessarily the formation of an ash plume. There are two distinct types of volcanic electrical discharges: volcanic lightning and continual radio frequency (CRF) impulses. T
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Longobardi, Mariantonietta <1983&gt. "Locating the source of volcanic tremor at stromboli volcano, italy." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amsdottorato.unibo.it/5181/1/Tesi.pdf.

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We have developed a method for locating sources of volcanic tremor and applied it to a dataset recorded on Stromboli volcano before and after the onset of the February 27th 2007 effusive eruption. Volcanic tremor has attracted considerable attention by seismologists because of its potential value as a tool for forecasting eruptions and for better understanding the physical processes that occur inside active volcanoes. Commonly used methods to locate volcanic tremor sources are: 1) array techniques, 2) semblance based methods, 3) calculation of wave field amplitude. We have choosen the third ap
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Longobardi, Mariantonietta <1983&gt. "Locating the source of volcanic tremor at stromboli volcano, italy." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amsdottorato.unibo.it/5181/.

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We have developed a method for locating sources of volcanic tremor and applied it to a dataset recorded on Stromboli volcano before and after the onset of the February 27th 2007 effusive eruption. Volcanic tremor has attracted considerable attention by seismologists because of its potential value as a tool for forecasting eruptions and for better understanding the physical processes that occur inside active volcanoes. Commonly used methods to locate volcanic tremor sources are: 1) array techniques, 2) semblance based methods, 3) calculation of wave field amplitude. We have choosen the third ap
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NOGUEIRA, LAGES Joao Pedro. "Constrains on mantle, slab and crustal contributions to major volatiles and noble gases along the Andean Volcanic Belt." Doctoral thesis, Università degli Studi di Palermo, 2020. http://hdl.handle.net/10447/395502.

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Books on the topic "Volcanic"

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Jean-Claude, Thouret, Chester David K, Ollier Cliff, Joyce B, and International Association of Geomorphology. Working Group on "Volcanic Geomorphology"., eds. Volcanic landforms, processes and hazards. Gebrüder Borntraeger, 2005.

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Ewert, John W. An assessment of volcanic threat and monitoring capabilities in the United States: Framework for a national volcano early warning system. U.S. Geological Survey, 2005.

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Groppelli, Gianluca. Stratigraphy and geology of volcanic areas. Geological Society of America, 2010.

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Groppelli, Gianluca. Stratigraphy and geology of volcanic areas. Geological Society of America, 2010.

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Tilling, I., ed. Volcanic Hazards. American Geophysical Union, 1989. http://dx.doi.org/10.1029/sc001.

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Gasparini, Paolo, Roberto Scarpa, and Keiiti Aki, eds. Volcanic Seismology. Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77008-1.

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Latter, John H., ed. Volcanic Hazards. Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-73759-6.

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Gottsmann, Joachim, Jürgen Neuberg, and Bettina Scheu, eds. Volcanic Unrest. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-58412-6.

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Dobran, Flavio. Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8.

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Rouwet, Dmitri, Bruce Christenson, Franco Tassi, and Jean Vandemeulebrouck, eds. Volcanic Lakes. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-36833-2.

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Book chapters on the topic "Volcanic"

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Németh, Károly. "Volcanic Geoheritage in the Light of Volcano Geology." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_1.

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AbstractVolcanic geoheritage relates to the geological features of a region that are associated with the formation of a volcanic terrain in diverse geoenvironmental conditions. These features include the volcanic processes, volcanic landforms and/or the eruptive products of volcanism that form the geological architecture of that region. Volcanic geoheritage is expressed through the landscape and how it forms and evolves through volcanic processes on various spatio-temporal scales. In this sense it is directly linked to the processes of how magma released, transported to the surface and fragmen
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Gill, Jim. "Island Arc Volcanism, Volcanic Arcs." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_20-2.

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Gill, Jim. "Island Arc Volcanism, Volcanic Arcs." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_20.

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Schmincke, Hans-Ulrich. "Volcanic Edifices and Volcanic Deposits." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_9.

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Dobran, Flavio. "Overview of Volcanic Processes." In Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_1.

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Dobran, Flavio. "Foundations of Transport Theory." In Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_2.

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Dobran, Flavio. "Properties of Igneous Materials." In Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_3.

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Dobran, Flavio. "Mantle Convection and Melt Segregation." In Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_4.

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Dobran, Flavio. "Magma Chambers." In Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_5.

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Dobran, Flavio. "Magma Ascent in Conduits." In Volcanic Processes. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-0647-8_6.

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Conference papers on the topic "Volcanic"

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Scollo, Simona, Luigi Mereu, Michele Prestifilippo, and Francesco Romeo. "Characterization of Volcanic Plumes by Remote Sensing Sensors: An Example from Etna Volcano." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10642244.

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Kumar, Ajay, Isha Dev, Priyanka, and Gulab Singh. "Volcanic Deformation Assessment Using SBAS-Insar and PS-Insar: Kīlauea Volcano Case Study." In 2024 IEEE India Geoscience and Remote Sensing Symposium (InGARSS). IEEE, 2024. https://doi.org/10.1109/ingarss61818.2024.10984271.

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Hou, Dongmei, Chao Li, Pengyu Gao, Xun Yuan, Xiaolong Zhang, and Zhong Cheng. "Sedimentary Evolution of Delta and Reservoir Distribution Under the Control of a Volcanic System." In ADIPEC. SPE, 2023. http://dx.doi.org/10.2118/215985-ms.

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Abstract The BZ34-9 oilfield is a clastic reservoir discovered in the Oligocene strata in the southern part of the Bohai Bay Basin. The volcanic system here is intermixed with a clastic reservoir that spans more than 1000 meters. In its upper part, it overlies about 2000 meters of Miocene strata. Volcanic activity has influenced the deposition and filling of the lacustrine and played a key role in controlling the distribution of clastic reservoirs. Based on 3D seismic data and lithological data from 74 wells, four types of volcanic were identified and extracted according to seismic sequences.
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Septama, E. "Java Volcanic Arc, what lies beneath?" In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-257.

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Java Island is an active volcanic arc that resides in the southwestern - southern boundary of Sundaland edges. The volcanic arc consists of several volcanism episodes, with a relatively younging trend northward (Late Oligocene to Pleistocene), following the Indo-Australian plates inward migration. In contrast to the prolific neighboring Northwest and Northeast Java Basins in the Northern edges of Java Island; the basin reconstruction and development in the East-West trending depression in median ranges of Java (from Bogor to Kendeng Troughs) are overlooked and lays bare the challenge to the se
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Hadiyanto, Imam Fikri, Dina Hanifah, and Wildan Nur Hamzah. "Distribution of Volcanic Rocks Porosity of Dissected Kromong Paleovolcano: Analogue of Volcanic Reservoir." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21240-ms.

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Abstract The potentiality of unconventional play on the volcanic reservoir was evaluated for the purpose to deliver an integrated evaluation of shallow reservoir target associated with the Northwest Java Basin (NWJB). This study provides basis discovery for further exploration and dissemination of volcanic reservoir by presenting an overview of geometric and porosity type analysis of Kromong paleo-volcano complex deposits associated with the NWJB comprehensively. Furthermore, reservoir lithofacies and pore space deployment of Kromong volcanic deposits were studied. The detailed lithofacies ana
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le Roux, Petrus, Gabriela Guzmán-Marusic, Osvaldo González-Maurel, Camila Pineda, Inés Rodríguez, and Benigno Godoy. "Contrasting old and young volcanism in Irruputuncu volcano, Central Andean Volcanic Zone, Chile." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.20472.

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Valero, Francisco P. J., Thomas P. Ackerman, and Walter L. Starr. "Changes in Solar Heating Rates and Planetary Albedo Induced by the El Chichon Volcanic Cloud." In Optical Remote Sensing. Optica Publishing Group, 1985. http://dx.doi.org/10.1364/ors.1985.wc4.

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The eruption of the Mexican volcano El Chichon (17.33°N, 93.20°W) on March 28, April 3, and April 4, 1982 injected particulate and gaseous matter into the stratosphere. This volcanic cloud ranked as one of the most massive of this century. DeLuisi et al, (1983) reported that "the atmospheric radiative effects of the El Chichon cloud far exceed the effects of all other volcanic clouds observed at Mauna Loa since observations were began in 1958". Very large optical depths were reported for this volcanic cloud in the northern tropics during the first few months since its formation.
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Satyana, A. H. "Trilogy Of Southeast Sundaland Terranes: Re-Uniting Drifted Terranes of Southeast Sundaland Using Common Marker ff The Late Cretaceous Volcanics to Volcanic-Clastics of The Meratus Mountains, South Sulawesi, And Sumba - Implications For Petroleum Opportunities." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-39.

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Amalgamation and dispersion of terranes characterized the growth and slivering of Southeast Sundaland into the present configuration of central Indonesia. Amalgamation of the Paternoster-West Sulawesi terrane which docked, in mid-Cretaceous time, onto the Southwest Borneo terrane, thus closed the Meso-Tethys Ocean at the Meratus suture. This made Sundaland expand its area to the east and southeast. In the Late Cretaceous time, the Ceno-Tethys oceanic plate subducted beneath Southeast Sundaland, giving rise to coeval volcanism in the Meratus Mountains and the surrounding areas. Dispersion of so
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Asgary, Ali. "Holovulcano: Augmented Reality simulation of volcanic eruptions." In The 8th International Defence and Homeland Security Simulation Workshop. CAL-TEK srl, 2018. http://dx.doi.org/10.46354/i3m.2018.dhss.007.

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"This paper describes an interactive holographic simulation of volcanic eruption. The aim of the project is to use Augmented Reality (AR) technology to visualize different volcanic eruptions for public education, emergency training, and preparedness planning purposes. To achieve this goal, a 3D model of the entire Vulcano Island in Italy has been created using real elevation data. Unity game engine and Microsoft Visual Studio have been used to develop HoloVulcano augmented/virtual reality simulation application. The current version of HoloVulcano simulates normal and unrest situations, single
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Yamano, Hidemasa, Hiroyuki Nishino, Kenichi Kurisaka, et al. "Development of Risk Assessment Methodology of Decay Heat Removal Function Against Natural External Hazards for Sodium-Cooled Fast Reactors: Project Overview and Volcanic PRA Methodology." In 2016 24th International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/icone24-60023.

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This paper describes mainly volcanic probabilistic risk assessment (PRA) methodology development for sodium-cooled fast reactors in addition to the project overview. In the volcanic PRA, only the effect of volcanic tephra (ash) was taken into account because there is a great distance between a plant site assumed in this study and volcanos. The volcanic ash could potentially clog air filters of air-intakes that are essential for the decay heat removal. The degree of filter clogging can be calculated by atmospheric concentration of ash and tephra fallout duration and also suction flow rate of ea
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Reports on the topic "Volcanic"

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Edwards, B. R., J. K. Russell, R. G. Anderson, and M. Harder. Overview of Neogene to Recent volcanism in the Atlin volcanic district, Northern Cordilleran volcanic province, northwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214025.

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Kirkham, R. V. Volcanic redbed copper. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/207986.

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Gandhi, S. S., and R. T. Bell. Volcanic-associated uranium. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/207992.

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Sherlock, R. L., and D. W. Lindsay. Volcanic stratigraphy of the QSP area, Hope Bay volcanic belt, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213182.

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Souther, J. G. Chapter 14: Volcanic Regimes. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134103.

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Rogers, N. Geochemistry of volcanic rocks. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/223356.

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Skulski, T., W. R. A. Baragar, J. Bédard, et al. Geochemistry of volcanic suites. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/223371.

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Hickson, C. J., and B. R. Edwards. Volcanoes and volcanic hazards. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212217.

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Wilson, A. M., J. K. Russell, M. C. Kelman, and C. J. Hickson. Geology of the Monmouth Creek volcanic complex, Garibaldi volcanic belt, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/298798.

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Goff, Fraser, Shari A. Kelley, Cathy J. Goff, et al. Geologic Map of Mount Taylor Volcano Area, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 2019. http://dx.doi.org/10.58799/gm-80.

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The Geologic Map of the Mount Taylor Volcano Area, New Mexico is a 1:36,000 compilation of six recent NMBGMR 1:24,000 geologic quadrangles that encompass this extinct composite stratovolcano. Mount Taylor is New Mexico's second-largest volcano after the Valles Caldera in the Jemez Mountains. This timely map and accompanying report, resulting from over a decade of thorough work, synthesizes the current geologic understanding of such an important landscape feature of the state.For such a complex volcanic landform, the report provides an exhaustive description of the volcano area in an easy-to-re
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