Дисертації з теми "Volcanic areas"
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Wang, Yunshuen. "Petrology ot Tertiary (?) Volcanic Rocks of Snowville Area, Utah, and Tertiary-Quaternary (?) Volcanic Rocks of Table Mountain and Holbrook Areas, Idaho." DigitalCommons@USU, 1985. https://digitalcommons.usu.edu/etd/3830.
Повний текст джерелаPistorio, Antonio. "Experimental and Computational Approaches to Enhance the Gravimetric Monitoring of Volcanic Areas." Doctoral thesis, Università di Catania, 2013. http://hdl.handle.net/10761/1308.
Повний текст джерелаGAGLIANO, Antonina Lisa. "Gaseous emissions from geothermal and volcanic areas: focus on methane and methanotrophs." Doctoral thesis, Università degli Studi di Palermo, 2014. http://hdl.handle.net/10447/90855.
Повний текст джерелаYearly, 22 Tg of CH4 are released in to the atmosphere from several natural and anthropogenic sources. Methane plays an important role in the Earth’s atmospheric chemistry and radiative balance being the most important greenhouse gas after carbon dioxide. Volcanic/geothermal areas contribute to the methane flux, being the site of widespread diffuse degassing of endogenous gases. Preliminary studies estimated a total CH4 emission from European geothermal and volcanic systems in the range 4-16 kt a-1. This estimate was obtained indirectly from CO2 or H2O output data and from CO2/CH4 or H2O/CH4 values measured in the main gaseous manifestations. The total estimated CH4 emission from geothermal/volcanic areas is still not well defined since the balance between emission through degassing and consumption through soil microbial oxidation is poorly known. Moreover, methane soil flux measurements are laboratory intensive and very few data have been collected until now in these areas. Such methods, although acceptable to obtain order-of-magnitude estimates, completely disregards possible methane microbial oxidation within the soil carried on by the methanotrophs. At the global scale, microbial oxidation in soils contributes for about 3-9% to the total removal of methane from the atmosphere. But the importance of methanotrophic organisms is even larger because they oxidize the greatest part of the methane produced in the soil and in the subsoil before its emission to the atmosphere. Environmental conditions in the soils of volcanic/geothermal areas (i.e. low oxygen content, high temperature and proton activity, etc.) have long been considered inadequate for methanotrophic microorganisms. But recently, it has been demonstrated that methanotrophic consumption in soils occurs also under such harsh conditions due to the presence of acidophilic and thermophilic Verrucomicrobia. These organisms were found in Italy at the Solfatara at Pozzuol (Italy), at Hell’s Gate (New Zealand) and in Kamchatka (Russia), pointing to a worldwide distribution. Here we report on methane oxidation rate measured in Pantelleria Island (Italy), Vulcano Island (Italy), Sousaki (Greece), Nea Kameni (Santorini) and Nisyros (Greece) soils. Clues of methane microbial oxidation in soils of these areas can be already found in the CH4/CO2 ratio of the flux measurements which is always lower than that of the respective fumarolic manifestations indicating a loss of CH4 during the travel of the gases towards earth’s surface. Laboratory methane consumption experiments made on soils collected at Pantelleria, Vulcano, Nea Kameni, Nysiros and Sousaki revealed for most samples consumption rates up to 950, 48, 15, 39 and 520 ng CH4 h-1 for each gram of soil (dry weight), respectively. Only few soil samples displayed no methane consumption activity. Analysis on soil gases and chemical-physical characteristics of the soils allowed us to discriminate the main factors that influenced the methanotrophs presence and the methane consumption rate. Soil gases composition, and in particular the amount of the CH4 and H2S, represent the main discriminating factor for methanotrophs. In fact, Vulcano and Nisyros Island, whose soil gas contained up to 250000 ppm of H2S, showed the lowest consumption rate. Moreover, in geothermal/volcanic soils H2S contribute to the soil pH lowering; highest methane consumption were recorded in Pantelleria island were H2S is less than 20 ppm and pH close to the neutrality were measured. Microbiological and molecular analyses allowed to detect the presence of methanotrophs affiliated to Gamma and Alpha-Proteobacteria and to the newly discovered acido-thermophilic methanotrophs belong to the Verrucomicrobia phylum in soils from Pantelleria. Culturable methanotrophic Alphaproteobacteria of the genus Methylocystis and the Gammaproteobacteria Methylobacterium were isolated by enrichment cultures. The isolates show a wide range of tolerance to pH and temperatures and an average methane oxidation rate up to 450 ppm/h. A larger diversity of (α- and γ-) proteobacterial and verrucomicrobial methanotrophs was detected by a culture-independent approach based on the amplification of the methane mono-oxygenase gene pmoA. This is the first report describing coexistence of both the methanotrophic phyla (Verrucomicrobia and Protebacteria) in the same geothermal site. The presence of proteobacterial methanoptrophs, in fact, was quite unexpected because they are generally considered not adapted to live in such harsh environments and could be explained by not really low pH values (> 5) of this specific geothermal site. Such species could have found their niches in the shallowest part of the soils of Favara Grande were the temperatures are not so high and thrive on the abundant upraising methane. Understanding the ecology of methanotrophy in geothermal sites will increase our knowledge of their role in methane emissions to the atmosphere.
Strauss, Simon Yale. "Marginal protection : sustainable development, social resilience and migration within natural protected areas of the Trans-Mexican Volcanic Belt, central Mexico." Thesis, McGill University, 2006. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=99609.
Повний текст джерелаCorcoran, Patricia Lynn. "Physical volcanology, geochemistry, and tectonic evolution of three selected areas in the Point Lake and Beaulieu River volcanic belts, Slave Province, Northwest Territories, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp05/NQ66650.pdf.
Повний текст джерелаChristianson, Amy Nadine. "Assessing and improving the effectiveness of staff training and warning system response at Whakapapa and Turoa ski areas, Mt. Ruapehu." Thesis, University of Canterbury. Geological Sciences, 2006. http://hdl.handle.net/10092/1271.
Повний текст джерелаOkubo, Ayako. "Studies on geomagnetic spatial and temporal variations in volcanic area." 京都大学 (Kyoto University), 2005. http://hdl.handle.net/2433/145088.
Повний текст джерела0048
新制・課程博士
博士(理学)
甲第11320号
理博第2878号
新制||理||1430(附属図書館)
22963
UT51-2005-D71
京都大学大学院理学研究科地球惑星科学専攻
(主査)教授 田中 良和, 教授 大志万 直人, 教授 鍵山 恒臣
学位規則第4条第1項該当
Spedalieri, Giancarlo. "Unravelling volcanic tremor source at mount etna from quantitative multiparametric analysis and moment tenso inversion." Doctoral thesis, Università di Catania, 2019. http://hdl.handle.net/10761/4134.
Повний текст джерелаLeahy, Kevin. "The geology of kimberlites from the Fort a la Corne area, Saskatchewan, Canada." Thesis, University of Leeds, 1996. http://etheses.whiterose.ac.uk/283/.
Повний текст джерелаThorkelson, Derek John Carleton University Dissertation Geology. "Volcanic and tectonic evolution of the Hazelton group in Spatsizi river (104H) map-area, north-central British Columbia." Ottawa, 1992.
Знайти повний текст джерелаDavarpanah, Armita. "Magmatic Evolution of the Eocene Volcanic Rocks of the Bijgerd Kuh E Kharchin Area, Uromieh-Dokhtar Zone, Iran." Digital Archive @ GSU, 2009. http://digitalarchive.gsu.edu/geosciences_theses/19.
Повний текст джерелаBarton, David J. "Frequency-magnitude distribution and spatial fractal dimension of seismicity at The Geysers geothermal area and Long Valley Caldera, California." Thesis, Durham University, 1998. http://etheses.dur.ac.uk/5046/.
Повний текст джерелаGunning, Michael H. "Definition and interpretation of Paleozoic volcanic domains, northwestern Stikinia, Iskut River Area, British Columbia." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/nq21289.pdf.
Повний текст джерелаNjilah, Isaac Konfor. "Geochemistry and petrogenesis of tertiary-quaternary volcanic rocks from Oku-Ndu area, N.W. Cameroon." Thesis, University of Leeds, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305536.
Повний текст джерелаCafaggi, Sara. "Temporal and geochemical characterization of the Negros de Aras (northern Chile) monogenetic volcanic field." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2021.
Знайти повний текст джерелаMilluzzo, Vincenzo. "Seismic chacterization of Vulcano island and Aeolian area by tectonic and seismo-volcanic events." Doctoral thesis, Università di Catania, 2013. http://hdl.handle.net/10761/1330.
Повний текст джерелаMalandrino, Pasqualino. "Il cancro tiroideo in Sicilia: rischio ambientale vulcanico." Doctoral thesis, Università di Catania, 2014. http://hdl.handle.net/10761/1577.
Повний текст джерелаSo, Chak-tong Anthony, and 蘇澤棠. "Petrology and geochemistry of volcanic rocks of the Lantau Peak Area, Lantau Island, Hong Kong." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31221646.
Повний текст джерелаArslan, Mehmet. "Mineralogy, geochemistry, petrology and petrogenesis of the Meydan-Zilan (Ercis-Van, Turkey) area volcanic rocks." Thesis, University of Glasgow, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.437611.
Повний текст джерелаBowen, Michael Peter. "The petrogenesis of the volcanic rocks of the Witwatersrand triad in the Klerksdorp area, Transvaal." Thesis, Rhodes University, 1985. http://hdl.handle.net/10962/d1001569.
Повний текст джерелаSo, Chak-tong Anthony. "Petrology and geochemistry of volcanic rocks of the Lantau Peak Area, Lantau Island, Hong Kong /." Hong Kong : University of Hong Kong, 1999. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21375549.
Повний текст джерелаAranzulla, Massimo. "Atmospheric water vapour tomography for DInSAR application and effect of volcanic plume on the microwaves." Doctoral thesis, Università di Catania, 2014. http://hdl.handle.net/10761/1543.
Повний текст джерелаPan, Jason J. "A geological and geochemical transect of the volcanic stratigraphy in the D'Alembert-Cléricy area, Noranda, Québec /." Thesis, McGill University, 1993. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=69648.
Повний текст джерелаChemostratigraphic units were established using Zr/Y, La$ sb{ rm N}$/Yb$ sb{ rm N}$, and other immobile and incompatible HFSE ratios, and AFM and Miyashiro major element plots. Lithogeochemical technique based on the HFSE and other immobile and incompatible elements have been applied to both fresh and altered rocks; the trace element parameters are more specific than the major element discriminants.
The stratigraphy along the D'Alembert-Clericy transect is subdivided into three major chemostratigraphic units: Lower Transitional Series, Middle Tholeiitic Series, and Upper Mixed Tholeiitic-Transitional Series. Overall, the lithologies comprise $ sim$65% tholeiitic and $ sim$35% transitional volcanics. The tholeiites are mainly represented by basalts and rhyolites, whereas the transitional rocks are mostly andesites and rhyolites.
The geological, stratigraphic, and lithochemical attributes along the transect indicate the potential for massive sulfide deposits is comparable to that of the Central Mine Sequence. Although the thesis area contains a greater proportion of basalts and volcaniclastic material than the Central Mine Sequence, both areas contain major tholeiite basalt-rhyolite bimodal sequences, several thick felsic units, and andesite-rhyolite transitional suites.
Bowen, Teral Barbara. "The geochemical stratigraphy of the volcanic rocks of the Witwatersrand triad in the Klerksdorp area, Transvaal." Thesis, Rhodes University, 1985. http://hdl.handle.net/10962/d1004932.
Повний текст джерелаCamire, Genevieve Carleton University Dissertation Geology. "Volcanic stratigraphy in the Hunter Creek Fault area, east of the Flavrian Pluton, Rouyn-Noranda, Quebec." Ottawa, 1989.
Знайти повний текст джерелаParadis, Suzanne Carleton University Dissertation Geology. "Stratigraphy, volcanology and geochemistry of the New Vauze - Norbec area, Central Noranda Volcanic Complex, Quebec, Canada." Ottawa, 1990.
Знайти повний текст джерелаHickson, Catherine Jean. "Quaternary volcanism in the Wells Gray-Clearwater area, east central British Columbia." Thesis, University of British Columbia, 1986. http://hdl.handle.net/2429/27315.
Повний текст джерелаScience, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
Aliotta, Marco Antonio. "Data mining techniques on volcano monitoring." Doctoral thesis, Università di Catania, 2013. http://hdl.handle.net/10761/1364.
Повний текст джерелаWright, Daniel Frederick. "Evaluating volcanic-hosted massive sulphide favourability using GIS-based spatial data integration models, Snow Lake area, Manitoba." Thesis, University of Ottawa (Canada), 1996. http://hdl.handle.net/10393/10064.
Повний текст джерелаGerlach, David Christian. "Geochemistry and petrology of recent volcanics of the Puyehue-Cordon Caulle Area, Chile (40.5S̊)." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/60119.
Повний текст джерелаMicrofiche copy available in Archives and Science.
Folded map in pocket at back of thesis.
Bibliography: leaves 369-388.
by David Christian Gerlach.
Ph.D.
Heikura, A. (Antti). "The volcanic rocks of the Länkipohja-Jämsä area in the southern part of the Central Finland Granitoid Complex." Master's thesis, University of Oulu, 2017. http://urn.fi/URN:NBN:fi:oulu-201704251579.
Повний текст джерелаIngalls, Andrew. "Reconnaissance Cenozoic volcanic geology of the Little Goose Creek area, northeastern Elko County, NV with an emphasis on the Jarbidge Rhyolite." Thesis, Kansas State University, 2014. http://hdl.handle.net/2097/18195.
Повний текст джерелаDepartment of Geology
Matthew Brueseke
The Little Goose Creek area is located in Elko County, Nevada just south of the central Snake River Plain and in the northeastern Great Basin. During the Miocene, northeastern Nevada was characterized by volcanism as well as prevalent extension and basin development, including widespread occurrences of porphyritic quartz-phyric silicic lavas and domes (e.g., the Jarbidge Rhyolite), ash-flow tuffs, and basaltic volcanism. Recent workers (e.g., Colgan and Henry, 2010) have provided new constraints on the timing of extension in the northern Great Basin (U.S.A.) and indicate that much of it occurred in the mid-Miocene. Other recent work has provided new temporal and petrologic constraints on 16.1 to 15.0 Ma Jarbidge Rhyolite volcanism in the northern Great Basin west of our study area, and suggest that it is intimately linked (spatially and temporally) with the aforementioned extension. This study aims to: [1] understand the spatiotemporal link between the volcanism in the northeastern Nevada study area and potentially correlative volcanism regionally (e.g., Jarbidge Rhyolite and explosive deposits associated with the <13 Ma Bruneau-Jarbidge or Twin Falls eruptive centers); [2] determine if the sampled Jarbidge Rhyolite lavas are chemically similar to those in and around Jarbidge, Nevada. In the Goose Creek area, we report a new laser [superscript]40Ar/[superscript]39Ar age for sanidine of 13.6 ± 0.03 Ma for a crystal-poor rhyolite lava (Rock Springs Rhyolite) and a Jarbidge Rhyolite lava (13.827±0.021 Ma) as well as an age on Jarbidge Rhyolite in Wells, NV (15.249±0.040 Ma) and West Wendover, NV (13.686±0.034 Ma). These lava samples, as well as sampled ash-flow tuffs from the Goose Creek region, plot within the A-type field on discrimination diagrams. The ash-flow tuffs are younger than the Rock Springs Rhyolite based on stratigraphic relationships and are sourced from both the Twin Falls eruptive center as well as the Bruneau Jarbidge eruptive center of the central Snake River Plain based on geochemical analysis. Also, a sequence of basaltic lavas crop out in the Goose Creek drainage; these basalts have ~43 wt.% silica and are chemically similar to <8 Ma olivine tholeiite basalts that crop out to the north, along the southwestern side of the Cassia Mountains, Idaho. These results, field relationships, and prior geological mapping suggest that the lavas and ash-flow tuffs erupted into active extensional basins.
O'Brien, Jeremy Mark. "Hydrogeochemical Characteristics of the Ngatamariki Geothermal Field and a Comparison with the Orakei Korako Thermal Area, Taupo Volcanic Zone, New Zealand." Thesis, University of Canterbury. Geological Sciences, 2010. http://hdl.handle.net/10092/4097.
Повний текст джерелаMoe, Aung. "Structural development of a volcanic sequence of the Lahn area during the variscan orogeny in the Rhenohercynian belt (Germany)." [S.l. : s.n.], 2000. http://deposit.ddb.de/cgi-bin/dokserv?idn=961466162.
Повний текст джерелаLees, Katherine Roisin. "Magmatic and tectonic changes through time in the Neogene volcanic rocks of the Vale area, Oregon, north western USA." Thesis, Open University, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261042.
Повний текст джерелаMercer, Lonnie T. "Geology of the Tierras Blancas Area in the Southeastern Acambay Graben, Central Mexico." BYU ScholarsArchive, 2005. https://scholarsarchive.byu.edu/etd/303.
Повний текст джерелаYurtmen, Sema. "Petrological and geochemical studies of Pre-Cretaceous metamorphic and Pliocene volcanic rocks in the area of northeast of Nigde, Turkey." Thesis, Keele University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296022.
Повний текст джерелаHanna, Teresa Rae. "Areal Extent and Volumes of the Dinner Creek Tuff Units, Eastern Oregon Based on Lithology, Bulk Rock Composition and Feldspar Mineralogy." PDXScholar, 2018. https://pdxscholar.library.pdx.edu/open_access_etds/4346.
Повний текст джерелаRuch, Joël. "Volcano deformation analysis in the Lazufre area (central Andes) using geodetic and geological observations." Phd thesis, Universität Potsdam, 2010. http://opus.kobv.de/ubp/volltexte/2010/4736/.
Повний текст джерелаVulkanische Deformationen in großem Maßstab, die mittels InSAR gemessen wurden, liefern neue Informationen und dadurch einen neuen Blickwinkel auf vulkan-tektonische Aktivitäten und das Verständnis von langlebigen, magmatischen Systemen. Die Destabilisierung eines solchen Systems in der Tiefe beeinflusst dauerhaft die Oberfläche durch Versatz des Bodens, magmatische Einflüsse und vulkanische Unruhen. Mit der Kombination aus kleinräumigem Bodenversatz gemessen mittels InSAR, numerischer Modellierung und langfristigen geologischen Beobachtungen, analysieren wir die Gegend um den Vulkan Lazufre in den Zentralanden, um die raumzeitliche Entwicklung der Region zu bestimmen. Bodenversatz wurde hierbei im Jahr 1997 mittels Radar-Interferrometrie (InSAR) gemessen, was eine Fläche von 1800 km² ausmacht, vergleichbar mit der Größe der Deformation des Kraters. Im Jahr 2000 wurde zusätzlich eine kleinräumige Deformation am Nachbarvulkan Lastarria entdeckt. Wir sehen räumliche als auch zeitliche Verbindungen zwischen der Deformation des Vulkans und vulkanischen Strukturen innerhalb der betroffenen Gegend. Wir folgern daraus, dass diese Beobachtungen der Ausdruck eines langlebigen, magmatischen Systems in der Tiefe an der Oberfläche sind. Es ist noch nicht klar, ob Lazufre größere vulkanische Unruhen, wie zum Beispiel Eruptionen auslösen könnte, aber die Deformation am Vulkan Lastarria und ein Anstieg der großräumigen Deformationsrate, machen diese Region interessant für eine zukünftige, kontinuierliche Überwachung.
Gisbert, Pinto Guillem. "The Miocene volcanism of the Sulcis area (SW Sardinia, Italy): Petrology, petrogenesis and geodynamic significance." Doctoral thesis, Universitat de Barcelona, 2012. http://hdl.handle.net/10803/84110.
Повний текст джерелаDurant l’Oligo-Miocè el funcionament en roll-back de la subducció sota el marge continental europeu de l’oest Mediterrani va provocar el desenganxament de la microplaca Sard-Corsa d’aquest marge i la seva migració primer amb una translació cap al SE i posteriorment amb una rotació en sentit antihorari fins a assolir la seva posició actual. Associada a aquest desplaçament es va produir l’obertura de la conca Liguro-Provençal en posició de back-arc. Com a resultat de la subducció es va produir abundant magmatisme calco-alcalí d’afinitat orogènica a l’illa de Sardenya. A la zona del Sulcis, al SW de Sardenya, el magmatisme va compartir inicialment les mateixes característiques que la resta del magmatisme sard, formant un apilament de doms i colades làviques de composicions andesítiques. Però cap als estadis finals del cicle magmàtic, els magmes generats van migrar de composició, donant lloc a un apilament d’unitats ignimbrítiques amb composicions majoritàriament riolítiques de transicionals a lleugerament alcalines. Malgrat la marcada diferència composicional entre la seqüència ignimbrítica del Sulcis i la resta del magmatisme Oligo-Miocè sard, aquesta va ser considerada com un exemple més d’aquest magmatisme. Per resoldre en part aquesta situació s’ha realitzat aquesta tesi. En aquest estudi s’ha revisat la seqüència vulcanoestratigràfica descrita així com les cartografies existents per tal de realitzar un mostreig sistemàtic de la seqüència ignimbrítica. L’estudi de les mostres recollides ha permès caracteritzar totes les unitats que formen la seqüència des del punt de vista de petrogràfic i geoquímic. Les dades obtingudes han permès desenvolupar una metodologia per al reconeixement de les unitats ignimbrítiques en base a la geoquímica de roca total, així com abordar l’estudi de la petrogènesi d’aquesta associació magmàtica. S’ha obtingut informació sobre l’àrea font dels magmes, que ha pogut ser caracteritzada, sobre els mecanismes de formació dels magmes estudiats i el seu significat geodinàmic, i sobre els processos que van controlar l’evolució dels magmes des de la seva formació fins a la seva expulsió en superfície en forma de materials volcànics.
Di, Stefan Agnese Giuseppa Federica. "Next generation of numerical models for inferring the volcano dynamics from geophysical observations." Doctoral thesis, Università di Catania, 2012. http://hdl.handle.net/10761/1074.
Повний текст джерелаHolroyd, Jonathan David. "The structure and stratigraphy of the Suardal area, Isle of Skye, northwest Scotland : an investigation of tertiary deformation in the Skye volcanic complex." Thesis, University of Manchester, 1994. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.659361.
Повний текст джерелаYoshikawa, Miyuki. "Seismic velocity structure beneath Otake-Hatchobaru geothermal area at Kuju Volcano in the central Kyusyu, Japan." 京都大学 (Kyoto University), 2004. http://hdl.handle.net/2433/147827.
Повний текст джерелаOswin, W. M. "Upper Devonian/lower carboniferous volcanism and mineralisation in the area east of the Rio Tinto mines, Iberian Pyrite Belt." Thesis, University of Southampton, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.375672.
Повний текст джерелаJones, Julie Amanda. "Geology of the Camboon volcanics in the Cracow area, Queensland : implications for the permo-carboniferous tectonic evolution of the New England fold belt /." [St. Lucia, Qld.], 2006. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe19453.pdf.
Повний текст джерелаKiuchi, Ryota. "New Ground Motion Prediction Equations for Saudi Arabia and their Application to Probabilistic Seismic Hazard Analysis." Kyoto University, 2020. http://hdl.handle.net/2433/253095.
Повний текст джерелаGiuffrida, Marisa. "Magma storage, ascent and degassing histories traced by textures and chemical zoning in crystals: application to the C02-Rich basaltic system of Mt. Etna Volcano." Doctoral thesis, Università di Catania, 2018. http://hdl.handle.net/10761/3632.
Повний текст джерелаGallagher, Brookie. "A comparative study of the Badger Pass igneous intrusion and the foreland volcanic rocks of the McDowell Springs area, Beaverhead county, Montana implications for the local late cretaceous sequence of events /." unrestricted, 2008. http://etd.gsu.edu/theses/available/etd-04212008-172506/.
Повний текст джерелаTitle from file title page. Timothy E. LaTour, committee chair; Hassan A. Babaie, Eirik J. Krogstad, William J. Fritz, committee members. Electronic text (111 p. : ill. (some col.), maps (some col.)) : digital, PDF file. Description based on contents viewed Aug. 20, 2008. Includes bibliographical references (p. 100-104).
Gallagher, Brookie Jean. "A Comparative Study of the Badger Pass Igneous Intrusion and the Foreland Volcanic Rocks of the McDowell Springs Area, Beaverhead County, Montana: Implications for the Local Late Cretaceous Sequence of Events." Digital Archive @ GSU, 2008. http://digitalarchive.gsu.edu/geosciences_theses/11.
Повний текст джерелаGrassi, Sabrina. "Characterization of active tectonic structures of the Etna volcano, through geophysical surveys, analysis of site response and deformation." Doctoral thesis, Università di Catania, 2017. http://hdl.handle.net/10761/3902.
Повний текст джерела