Auswahl der wissenschaftlichen Literatur zum Thema „Volcanis islands“
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Zeitschriftenartikel zum Thema "Volcanis islands"
Smellie, John L. „Chapter 3.2a Bransfield Strait and James Ross Island: volcanology“. Geological Society, London, Memoirs 55, Nr. 1 (2021): 227–84. http://dx.doi.org/10.1144/m55-2018-58.
Der volle Inhalt der QuelleMcDOUGALL, IAN. „Age of volcanism and its migration in the Samoa Islands“. Geological Magazine 147, Nr. 5 (10.02.2010): 705–17. http://dx.doi.org/10.1017/s0016756810000038.
Der volle Inhalt der QuelleSimurda, Christine, Lori A. Magruder, Jonathan Markel, James B. Garvin und Daniel A. Slayback. „ICESat-2 Applications for Investigating Emerging Volcanoes“. Geosciences 12, Nr. 1 (14.01.2022): 40. http://dx.doi.org/10.3390/geosciences12010040.
Der volle Inhalt der QuelleLeat, Philip T., und Teal R. Riley. „Chapter 3.1a Antarctic Peninsula and South Shetland Islands: volcanology“. Geological Society, London, Memoirs 55, Nr. 1 (2021): 185–212. http://dx.doi.org/10.1144/m55-2018-52.
Der volle Inhalt der QuelleGriffiths, Chris J., und Richard D. J. Oglethorpe. „The stratigraphy and geochronology of Adelaide Island“. Antarctic Science 10, Nr. 4 (Dezember 1998): 462–75. http://dx.doi.org/10.1017/s095410209800056x.
Der volle Inhalt der QuelleGeyer, A., D. Pedrazzi, J. Almendros, M. Berrocoso, J. López-Martínez, A. Maestro, E. Carmona, A. M. Álvarez-Valero und A. de Gil. „Chapter 7.1 Deception Island“. Geological Society, London, Memoirs 55, Nr. 1 (2021): 667–93. http://dx.doi.org/10.1144/m55-2018-56.
Der volle Inhalt der QuelleDimitrov, Dimitar, und Banush Banushev. „Geological-geomorphological characteristics and petrographical composition of the St. Anastasia Island“. Acta Scientifica Naturalis 8, Nr. 1 (01.03.2021): 118–25. http://dx.doi.org/10.2478/asn-2021-0010.
Der volle Inhalt der QuelleMutaqin, Bachtiar W., Muh Aris Marfai, Danang Sri Hadmoko, Franck Lavigne, Audrey Faral, Helvetia Wijayanti und Widiyana Riasasi. „Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)“. E3S Web of Conferences 325 (2021): 03012. http://dx.doi.org/10.1051/e3sconf/202132503012.
Der volle Inhalt der QuellePatrick, Matthew R., und John L. Smellie. „Synthesis A spaceborne inventory of volcanic activity in Antarctica and southern oceans, 2000–10“. Antarctic Science 25, Nr. 4 (12.06.2013): 475–500. http://dx.doi.org/10.1017/s0954102013000436.
Der volle Inhalt der QuelleMonjoie, Philippe, Henriette Lapierre, Artan Tashko, Georges H. Mascle, Aline Dechamp, Bardhyl Muceku und Pierre Brunet. „Nature and origin of the Triassic volcanism in Albania and Othrys: a key to understanding the Neotethys opening?“ Bulletin de la Société Géologique de France 179, Nr. 4 (01.07.2008): 411–25. http://dx.doi.org/10.2113/gssgfbull.179.4.411.
Der volle Inhalt der QuelleDissertationen zum Thema "Volcanis islands"
García, Pérez Olaya. „The explosive volcanism of Teide-Pico Viejo volcanic complex, Canary Island“. Doctoral thesis, Universitat de Barcelona, 2013. http://hdl.handle.net/10803/130923.
Der volle Inhalt der QuelleEl complejo volcánico Teide Pico Viejo (TPV) es un stratovolcano situado en la isla de Tenerife, Islas Canarias, y ha sido considerado por la UNESCO el sistema volcánico activo más peligroso en Europa. Los eventos explosivos en el complejo TPV se han limitado tradicionalmente a la erupción subplinian de Montaña Blanca, que ocurrió hace unos 2000 años. Una reciente revisión de la estratigrafía muestra que la actividad explosiva fonolítica asociada a TPV ha sido significativa durante el Holoceno, presentado distintos episodios relacionados con erupciones que varían en tamaño de estromboliano a sub-pliniano. A través de las correlaciones estratigráficas obtenidas mediante observaciones de campo y datos de mineralógicos y geoquímicos, se han identificado 11 erupciones explosivas fonolítica relacionados con los domos satélite presentes en todo complejo TPV. Una de las erupciones más representativa es El Boquerón (5660 YBP), un domo que generó un evento explosivo de VEI 3 con un volumen mínimo de 4-6x107 m3 y produjo una columna con una altura de hasta 9 kilometros sobre el nivel del mar ( MER 6.9-8.2x105 kg / s, durante 9-15 h). La ocurrencia de estos eventos explosivos en el reciente registro eruptivo del complejo TPV es de gran importancia para evaluar el riesgo impuesto por el complejo volcánico en Tenerife. Estas erupciones han generado una amplia gama de amenazas directas, como los depósitos de caida, emplazamiento de las corrientes piroclásticas densidad, flujo de derrubios, lahares y avalanchas de roca, lo que podría ocurrir de nuevo en caso de renovación de la actividad volcánica. Los resultados obtenidos en nuestro estudio son relevantes para definir escenarios eruptivos realista y precisos para el complejo TPV y para evaluar su riesgo asociado, un paso necesario en la evaluación y mitigación del riesgo volcánico en Tenerife
Maund, J. G. „The volcanic geology, petrology and geochemistry of Caldeira volcano, Graciosa, Azores, and its bearing on contemporaneous felsic-mafic oceanic island volcanism“. Thesis, University of Reading, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.370121.
Der volle Inhalt der QuelleLetham-Brake, Mark. „Geological constraints on fluid flow at Whakaari volcano (White Island)“. Thesis, University of Canterbury. Department of Geological Sciences, 2013. http://hdl.handle.net/10092/8728.
Der volle Inhalt der QuelleSigmarsson, Olgeir. „Geochimie isotopique du thorium des iles oceaniques (islande, canaries) et des zones de subduction (indonesie et chili)“. Clermont-Ferrand 2, 1990. http://www.theses.fr/1990CLF21284.
Der volle Inhalt der QuelleBelien, Isolde L. M. B. (Leo Maria Beatrijs) 1985. „Gas Migration Through Crystal-Rich Mafic Volcanic Systems and Application to Stromboli Volcano, Aeolian Islands, Italy“. Thesis, University of Oregon, 2011. http://hdl.handle.net/1794/12107.
Der volle Inhalt der QuelleCrystals influence the migration of gas through magma. At low concentrations, they increase the bulk fluid properties, especially viscosity. At concentrations close to maximum packing, crystals form a rigid framework and magma cannot erupt. However, erupted pyroclasts with crystal contents close to the packing concentration are common at mafic volcanoes that exhibit Strombolian behavior. In this dissertation, I study the influence of solid particles on gas migration. I apply my results to Stromboli volcano, Italy, type locality of the normal Strombolian eruptive style, where gas moves through an essentially stagnant magma with crystallinity ∼50%. Specifically, I investigate the effect of crystals on flow regime, gas content (Chapter II), bubble concentration (number densities), bubble shapes, bubble sizes (Chapter III), and bubble rise velocities (gas flux) (Chapter IV). I find that gas-liquid flow regimes are not applicable at high particle concentrations and should be replaced by new, three-phase (gas-liquid-solid) regimes and that degassing efficiency increases with particle concentration (Chapter II). In Chapter III, I show that crystals modify bubble populations by trapping small bubbles and causing large bubbles to split into smaller ones and by modifying bubble shapes. In Chapter IV, I model Stromboli's crystal-rich magma as a network of capillary tubes and show that bubble rise velocities are significantly slower than free rise velocities in the absence of particles. In each chapter, I use analogue experiments to study the effect of different liquid and solid properties on gas migration in viscous liquids. I then apply my analogue results to magmatic conditions using simple parameterizations and/or numerical modeling or by comparing the results directly to observations made on crystal-rich volcanic rocks. Chapter V proposes a mechanism for Strombolian eruptions and gas migration through the crystalrich magma in which the effect of crystals is included. This model replaces the current twophase "slug" model, which cannot account for the high crystallinity observed at Stromboli. There are three appendices in this dissertation: a preliminary study of the influence of particles on gas expansion, image analysis methods, and the numerical code developed in Chapter IV. This dissertation includes previously published and unpublished co-authored material.
Committee in charge: Katharine Cashman, Chairperson; Alan Rempel, Member; Mark Reed, Member; Raghuveer Parthasarathy, Outside Member
Dávila, Harris Pablo. „Explosive ocean-island volcanism : the 1.8–0.7 Ma explosive eruption history of Cañadas volcano recorded by the pyroclastic successions around Adeje and Abona, southern Tenerife, Canary Islands“. Thesis, University of Leicester, 2009. http://hdl.handle.net/2381/9931.
Der volle Inhalt der QuelleGrunewald, Uwe. „Measuring and modelling of volcanic pollutants from White Island and Ruapehu volcanoes assessment of related hazard in the North Island /“. Thesis, University of Canterbury. Geological Sciences, 2007. http://hdl.handle.net/10092/1428.
Der volle Inhalt der QuelleHevia, Cruz Francisco. „Climatic and landscape evolution of the Azores over the past million years“. Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ035.
Der volle Inhalt der QuelleLandscape evolution on volcanic islands is driven by complex interactions between volcano growth and destruction by a variety of processes (explosive eruptions, landslides, riverine erosion, weathering). Major climate changes, may impact the dynamics of degradation processes at different spatial and temporal scales. For example, extreme rain can produce an immediate hydrological response causing important destruction. Changes in weathering rates, sensitive to precipitation and temperature, can trigger changes in soil fertility but also modify global carbon cycling.The Azores volcanic islands provide an ideal setting to study these interactions, with both scientific and societal significance, especially in the context of ongoing global warming. Located in the Central North Atlantic, they are under the influence of major climatic drivers. Most of them had pulses of volcanic activity over the past 1 Myr, a period characterized by high-amplitude glacial-interglacial transitions with major climatic changes. While global climatic variations have been relatively well-studied for this period, reconstructing the atmospheric paleoclimate and its effects at local/regional scales remains challenging. Paleosols (PSs) are fossil soils formed by weathering at surface, and later incorporated into the geological record. Their geochemistry provides valuable insights into past environmental conditions, while the geochronology of volcanic products “bracketing” PSs allows their temporal constraint.In this work, we reconstructed mean annual precipitations (MAP) and air temperature (MAAT) over the last 1 Myr in the Azores region through a combined geochemical-geochronological study of PSs. Two proxies based on PSs’ major element were used: the weathering index (CIA-K) and the Clayeyness, both validated in other volcanic settings. The precise dating of volcanic units by either unspiked K-Ar on lava flow groundmass separates or ⁴⁰Ar/³⁹Ar on single K-feldspar of trachytic fallout evidence “pulses” of soil-formation within only a few kyr. This occurred especially after glacial terminations (MIS 21, 19, 11, 9e, 5e and 1), under wet and warm conditions. Fast paleoenvironmental changes were recorded in PSs’ geochemistry, and MAAT reconstructions (12-28 ᵒC) agree with previously published Sea Surface Temperatures, pointing to a tight ocean-atmosphere teleconnection. Those “pulses” suggest sustained weakening phases for the Azores High, allowing humid air currents (Westerlies) to reach further to the south.Our data also show contrasted rates of vertical soil development (3-180 mm/kyr). Weathering was favored by the structure and texture of parental materials, as PSs formed under lower MAP in pyroclastic deposits than in lava flows (~500 and ~800 mm/yr thresholds). This highlights the influence of fragmentation on weathering’s kinetics due to higher specific surface area. Enhanced weathering at surface and along geological discontinuities may have promoted mechanical weakening, favoring erosion and landslides. Notably, high MAPs (up to 1500 mm/yr) obtained around the Eemian interglacial stage are coincident in time with the initiation of a large slide complex on the southern flank of Pico. Intense precipitation may have led to increased water infiltration favoring enhanced hydromagmatic interactions. Drastic increase in pore pressure may then have triggered the initiation of the flank movement along listric faults that are still active. Current conditions in the Azores are wetter and slightly warmer than during the last Myr. Increased infiltration along faults could partly control subsequent movement and yield to detachment of the outer flank of Pico, with potentially dramatic consequences.More generally, present temperature and humidity increase on volcanic islands points to intense weathering, resulting in fast landscape evolution, increased lixiviation and elementary export and high atmospheric CO₂ uptaking, with local, regional and global impacts
Meletlidis, Tsiogalos Stavros. „Eruptive dynamics and petrological evolution of recent volcanism on the El Hierro Island : Implications for volcanic hazard assessment“. Doctoral thesis, Universitat de Barcelona, 2017. http://hdl.handle.net/10803/461582.
Der volle Inhalt der Quellea última erupción en la isla de El Hierro (2011-12) representa una excelente oportunidad para estudiar el volcanismo monogenético basáltico. La comparación de los productos emitidos durante esa erupción con los emitidos en erupciones anteriores y la interpretación de los resultados petrológicos junto con los datos obtenidos por la red multiparamétrica de vigilancia volcánica del IGN de vigilancia (estaciones sísmicas, GNSS, gravimétricas,…) nos ha permitido lograr un conocimiento integral de los procesos que ocurren antes y durante este tipo de erupciones basáticas monogenéticas, que son las más probables a corto y medio plazo en Canarias. Este enfoque multidisciplinar nos ha proporcionado nueva información sobre el ascenso del magma, las condiciones y procesos internos, los mecanismos de las erupciones basálticas, los mecanismos de deposición y los escenarios de interacción. La interpretación conjunta de todos los datos obtenidos permitirá una mejor evaluación del riesgo volcánico, no solo para la isla de El Hierro, sino para todo el archipiélago canario. En esta tesis, junto con el estudio de la erupción de 2011-12, se han estudiado dos más erupciones; la que ha dado el depósito de productos evolucionados en el centro de la isla (área del Malpaso) donde la dinámica y evolución de ella se ha ligado en la interacción magma/agua y la erupción de Chinyero (1909, Tenerife) que con rasgos similares a la de El Hierro (basáltica) pero con menor volumen de magma involucrado, ha tenido una dinámica más explosiva de lo que se había creído hasta hoy. Por lo tanto, las evaluaciones de riesgo volcánico a largo y corto plazo para el conjunto de las islas Canarias deben tener en cuenta posibles escenarios que no solo incluyen la erupciones basálticas submarinas, como es el caso de 2011-2012, sino también las erupciones sub-aéreas de corta vida como la del Chinyero o las erupciones como la del Malpaso, donde la intrusión basáltica y la interacción con el agua son procesos que aumentan la explosividad de una erupción y como consecuencia, al área afectado de sus productos.
Palmiotto, Camilla <1985>. „Transform Tectonics and Non-Volcanic Oceanic Islands“. Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2014. http://amsdottorato.unibo.it/6472/1/Palmiotto_Camilla_Tesi.pdf.
Der volle Inhalt der QuelleBücher zum Thema "Volcanis islands"
Greensmith, J. T. Lanzarote, Canary Islands. London: Geologists' Association, 2000.
Den vollen Inhalt der Quelle findenLuigina, Vezzoli, Hrsg. Island of Ischia. Roma: Consiglio nazionale delle ricerche, 1988.
Den vollen Inhalt der Quelle findenTagliaferro, Linda. How does a volcano become an island? London: Raintree, 2010.
Den vollen Inhalt der Quelle findenTagliaferro, Linda. How does a volcano become an island? Chicago, Ill: Raintree, 2008.
Den vollen Inhalt der Quelle findenK, Sako Maurice, Geological Survey (U.S.) und Northern Mariana Islands. Disaster Control Office, Hrsg. Volcanic investigations in the Commonwealth of the Northern Mariana Islands, April to May 1994. [Denver, CO]: U.S. Geological Survey, 1995.
Den vollen Inhalt der Quelle findenSigurjónsson, Sigurgeir. Volcano island. Reykjavík: Forlagið, 2010.
Den vollen Inhalt der Quelle findenD, Ayres L., und Geological Association of Canada, Hrsg. Pyroclastic volcanism and deposits of cenozoic intermediate to felsicvolcanic islands: With implications for precambrian greenstone-belt volcanoes. Ann Arbor: U.M.I., 1987.
Den vollen Inhalt der Quelle findenGill, Robin. Tenerife Canary Islands. 2. Aufl. London: The Geologists' Association, 2003.
Den vollen Inhalt der Quelle findenTait, Peter. White Island: New Zealand's most active volcano. Auckland, N.Z: Godwit, 2001.
Den vollen Inhalt der Quelle findenGreensmith, J. T. Lanzarote, Canary Islands. [London]: The Geologists' Association, 2000.
Den vollen Inhalt der Quelle findenBuchteile zum Thema "Volcanis islands"
Hernández Ramos, William, Victor Ortega, Monika Przeor, Nemesio M. Pérez und Pedro A. Hernández. „Submarine Eruption of El Hierro, Geotourism and Geoparks“. In Geoheritage, Geoparks and Geotourism, 115–23. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_11.
Der volle Inhalt der QuelleDóniz-Páez, Javier, und Rafael Becerra-Ramírez. „Geomorphosites of El Hierro UNESCO Global Geopark (Canary Islands, Spain): Promotion of Georoutes for Volcanic Tourism“. In Geoheritage, Geoparks and Geotourism, 87–93. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_8.
Der volle Inhalt der QuelleGuillén-Martín, Cayetano, und Carmen Romero. „Volcanic Geomorphology in El Hierro Global Geopark“. In Geoheritage, Geoparks and Geotourism, 33–42. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_3.
Der volle Inhalt der QuelleGill, Jim. „Island Arc Volcanism, Volcanic Arcs“. In Encyclopedia of Marine Geosciences, 1–7. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_20-2.
Der volle Inhalt der QuelleGill, Jim. „Island Arc Volcanism, Volcanic Arcs“. In Encyclopedia of Marine Geosciences, 379–83. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_20.
Der volle Inhalt der QuelleDe la Cruz-Modino, Raquel, Cristina Piñeiro-Corbeira, Shankar Aswani, Carla González-Cruz, David Domínguez, Paula Ordóñez García, Agustín Santana-Talavera und José Pascual-Fernández. „Cultural Seascapes in the ‘Sea of Calms’ and La Restinga Coast“. In Geoheritage, Geoparks and Geotourism, 105–13. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_10.
Der volle Inhalt der QuelleSchmincke, Hans-Ulrich. „Seamounts and Volcanic Islands“. In Volcanism, 71–96. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_6.
Der volle Inhalt der QuelleSchmieder, Robert William. „Volcanic features“. In Heard Island, 299–314. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-20343-5_12.
Der volle Inhalt der QuelleCasillas Ruiz, Ramón, Yurena Pérez Candelario und Cristina Ferro Fernández. „Geoheritage Inventory of the El Hierro UNESCO Global Geopark“. In Geoheritage, Geoparks and Geotourism, 43–51. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_4.
Der volle Inhalt der QuelleBeltrán-Yanes, Esther, und Isabel Esquivel-Sigut. „The Vegetation Landscapes of a Oceanic Recent Volcanic Island“. In Geoheritage, Geoparks and Geotourism, 53–63. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_5.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Volcanis islands"
Waibel, Al, und Adam Jones. „Near-Offshore Oceanic Geothermal Resources Developed from On-Shore Directional Drilling“. In Offshore Technology Conference. OTC, 2024. http://dx.doi.org/10.4043/35417-ms.
Der volle Inhalt der QuelleSeptama, 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.
Der volle Inhalt der QuelleИванов, А. Н. „TO THE QUESTION OF POLYSTRUCTURAL ORGANISATION OF LANDSCAPE SPACE“. In Геосистемы Северо-Восточной Азии. Crossref, 2021. http://dx.doi.org/10.35735/tig.2021.61.88.005.
Der volle Inhalt der QuelleAsgary, 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.
Der volle Inhalt der QuelleYanis, Muhammad, Zaini Nasrullah, Muhammad Isa, Ananda Riski, Muzakir Zainal und Andri Yadi Paembonan. „Optimizing the Gravity Data and Geological Observation for Mapping the Local Fault around the Jaboi Volcano“. In The 5th International Conference on Science and Technology Applications. Switzerland: Trans Tech Publications Ltd, 2024. http://dx.doi.org/10.4028/p-mezta6.
Der volle Inhalt der QuelleHanamuro, Takahiro, Ken-Ichi Yasue, Yoko Saito-Kokubu, Koichi Asamori, Tsuneari Ishimaru und Koji Umeda. „Current R & D Activities in the Study on Geosphere Stability“. In ASME 2010 13th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2010. http://dx.doi.org/10.1115/icem2010-40018.
Der volle Inhalt der QuelleNaidu, Som, Dhiraj Bhartu und Tony Mays. „Access to ICT Infrastructure and Devices in the South Pacific“. In Tenth Pan-Commonwealth Forum on Open Learning. Commonwealth of Learning, 2022. http://dx.doi.org/10.56059/pcf10.3503.
Der volle Inhalt der QuelleGodsey, Nick, Nichole Grau und Jenna Cookson. „Session 2.1 Jeju volcanic island and lava tubes“. In The 4th Global Virtual Conference of the Youth Environmental Alliance in Higher Education. Michigan Technological University, 2022. http://dx.doi.org/10.37099/mtu.dc.yeah-conference/dec2021/all-events/4.
Der volle Inhalt der QuelleVindas Umaña, Andrea, Jonathan Godinez, Jason Navarro Ulate, Cornelia Van Hazinga, Sara Mana und Paulo Ruiz. „LACK OF VOLCANIC LINEAMENTS AND ANISOTROPY IN VOLCANISM RELATED TO RIFTING IN EL HIERRO, CANARY ISLANDS - SPAIN“. In Northeastern Section-56th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021ne-361606.
Der volle Inhalt der QuelleSecrétan, Alexia, und Olivier Reubi. „Linking the sub-volcanic plutonic complex and the magmatic evolution at La Gomera volcano, Canary Islands.“ In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.17912.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Volcanis islands"
Tweet, Justin S., Vincent L. Santucci, Kenneth Convery, Jonathan Hoffman und Laura Kirn. Channel Islands National Park: Paleontological resource inventory (public version). National Park Service, September 2020. http://dx.doi.org/10.36967/nrr-2278664.
Der volle Inhalt der QuelleHaggart, J. W., L. T. Dafoe, K. M. Bell, G L Williams, E. T. Burden, L. D. Currie, R. A. Fensome und A. R. Sweet. Historical development of a litho- and biostratigraphic framework for onshore Cretaceous-Paleocene deposits along western Baffin Bay. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321828.
Der volle Inhalt der QuellePeterson, T. D., N. Wodicka, S J Pehrsson, P. Acosta-Gongora, V. Tschirhart, C. J. Jefferson, H. Steenkamp, E. Martel, J. Percival und D. Corrigan. The Rae Province at 2.6 Ga: a sanukitoid storm on the Canadian Shield, Nunavut. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332505.
Der volle Inhalt der QuelleNarvaez, Liliana, Joerg Szarzynski und Zita Sebesvari. Technical Report: Tonga volcano eruption. United Nations University - Institute for Environment and Human Security (UNU-EHS), August 2022. http://dx.doi.org/10.53324/ysxa5862.
Der volle Inhalt der QuelleBerndt, Christian. RV SONNE Fahrtbericht / Cruise Report SO277 OMAX: Offshore Malta Aquifer Exploration, Emden (Germany) – Emden (Germany), 14.08. – 03.10.2020. GEOMAR Helmholtz Centre for Ocean Research Kiel, Januar 2021. http://dx.doi.org/10.3289/geomar_rep_ns_57_20.
Der volle Inhalt der QuelleNye, C. J., W. E. Scott, O. K. Neill, C. F. Waythomas, C. E. Cameron und A. T. Calvert. Geology of Kasatochi volcano, Aleutian Islands, Alaska. Alaska Division of Geological & Geophysical Surveys, Juli 2017. http://dx.doi.org/10.14509/29718.
Der volle Inhalt der QuelleSaumur, B. M., M. C. Williamson und C. A. Evenchick. Volcanic-intrusive complexes of western Axel Heiberg Island. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/297374.
Der volle Inhalt der QuelleWilliamson, M. C., B. M. Saumur und C. A. Evenchick. HALIP volcanic-intrusive complexes, Axel Heiberg Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297491.
Der volle Inhalt der QuelleWilliamson, M. C., B. M. Saumur und C. A. Evenchick. HALIP volcanic-intrusive complexes, Axel Heiberg Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297784.
Der volle Inhalt der QuelleRobbins, S. D. Active volcanoes of Kamchatka and northern Kurile Islands. Alaska Division of Geological & Geophysical Surveys, Dezember 2010. http://dx.doi.org/10.14509/21141.
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