Relevant bibliographies by topics / Transport de magmas

Contents

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

Academic literature on the topic 'Transport de magmas'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Transport de magmas"

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Russell, J. Kelly, R. Stephen J. Sparks, and Janine L. Kavanagh. "Kimberlite Volcanology: Transport, Ascent, and Eruption." Elements 15, no. 6 (2019): 405–10. http://dx.doi.org/10.2138/gselements.15.6.405.

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Kimberlite rocks and deposits are the eruption products of volatile-rich, silica-poor ultrabasic magmas that originate as small-degree mantle melts at depths in excess of 200 km. Many kimberlites are emplaced as subsurface cylindrical-to-conical pipes and associated sills and dykes. Surficial volcanic deposits of kimberlite are rare. Although kimberlite magmas have distinctive chemical and physical properties, their eruption styles, intensities and durations are similar to conventional volcanoes. Rates of magma ascent and transport through the cratonic lithosphere are informed by mantle cargo
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Petford, Nick, Ross C. Kerr, and John R. Lister. "Dike transport of granitoid magmas." Geology 21, no. 9 (1993): 845. http://dx.doi.org/10.1130/0091-7613(1993)021<0845:dtogm>2.3.co;2.

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Weinberg, Roberto Ferrez. "Ascent mechanism of felsic magmas: news and views." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 87, no. 1-2 (1996): 95–103. http://dx.doi.org/10.1017/s0263593300006519.

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ABSTRACT:Diapirism has been discredited as a transport mechanism for magmas partly because diapirs seem to be unable to bring magmas to shallow crustal levels (&lt;10km) and partly because recent developments in the theory of dyke propagation have shown that sufficiently wide dykes are able to efficiently transport felsic magmas through the crust. However, it is still unclear how felsic dykes grow to widths that allow them to propagate faster than they close by magma freezing. Ultimately, it may be the ability of felsic dykes to grow within the source that controls which mechanism dominates as
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Geist, Dennis, William White, Terry Naumann, and Robert Reynolds. "Illegitimate magmas of the Galápagos: Insights into mantle mixing and magma transport." Geology 27, no. 12 (1999): 1103. http://dx.doi.org/10.1130/0091-7613(1999)027<1103:imotgp>2.3.co;2.

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Miller, Calvin F., E. Bruce Watson, and T. Mark Harrison. "Perspectives on the source, segregation and transport of granitoid magmas." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 79, no. 2-3 (1988): 135–56. http://dx.doi.org/10.1017/s0263593300014176.

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ABSTRACTThe pursuit of a comprehensive theory for the origin and evolution of granitoids is hindered by our incomplete understanding of the nature of the source and the mechanisms by which the magma is segregated and transported. This paper is a collection of three largely independent and necessarily incomplete perspectives on these outstanding issues. Lower to mid-crustal regions, which contain the principal source material for granitoid magmas, are highly heterogeneous. Consideration of available transfer mechanisms suggests that (1) this heterogeneity survives all foreseeable lower crustal
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Dingwell, D. B. "Transport Properties of Magmas: Diffusion and Rheology." Elements 2, no. 5 (2006): 281–86. http://dx.doi.org/10.2113/gselements.2.5.281.

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Macdonald, R., B. Bagiński, B. G. J. Upton, P. Dzierżanowski, W. Marshall-Roberts, and M. Prieto. "The Palaeogene Eskdalemuir dyke, Scotland: long-distance lateral transport of rhyolitic magma in a mixed-magma intrusion." Mineralogical Magazine 73, no. 2 (2009): 285–300. http://dx.doi.org/10.1180/minmag.2009.073.2.285.

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AbstractThe Palaeogene Eskdalemuir dyke, part of the Mull dyke swarm in the Southern Uplands of Scotland, is ~60 km long and up to 40 m thick. Its southern tip is 230 km from the inferred source on Mull. The dyke is composite, with tholeiitic basaltic margins and a vitreous central facies ranging from basaltic andesite to andesite in composition. Plagioclase and pyroxene phenocrysts and matrix crystals in the central facies show unusually large compositional ranges and complex textural relationships. Wholerock major and trace-element abundances show linear variations against MgO content, consi
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Paterson, Scott R., Nick Petford, Ross C. Kerr, and John R. Lister. "Dike transport of granitoid magmas: Comment and Reply." Geology 22, no. 5 (1994): 473. http://dx.doi.org/10.1130/0091-7613(1994)022<0473:dtogmc>2.3.co;2.

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Leat, Philip T. "On the long-distance transport of Ferrar magmas." Geological Society, London, Special Publications 302, no. 1 (2008): 45–61. http://dx.doi.org/10.1144/sp302.4.

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GAFFNEY, AMY M. "Environments of Crystallization and Compositional Diversity of Mauna Loa Xenoliths." Journal of Petrology 43, no. 6 (2002): 963–81. http://dx.doi.org/10.1093/petrology/43.6.963.

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Abstract Two picrite flows from the SW rift zone of Mauna Loa contain xenoliths of dunite, harzburgite, lherzolite, plagioclase-bearing lherzolite and harzburgite, troctolite, gabbro, olivine gabbro, and gabbronorite. Textures and olivine compositions preclude a mantle source for the xenoliths, and rare earth element concentrations of xenoliths and clinopyroxene indicate that the xenolith source is not old oceanic crust, but rather a Hawaiian, tholeiitic-stage magma. Pyroxene compositions, phase assemblages and textural relationships in xenoliths indicate at least two different crystallization
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Dissertations / Theses on the topic "Transport de magmas"

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MERIAUX, CATHERINE. "Transport de magmas dans les filons." Paris 7, 1996. http://www.theses.fr/1996PA077098.

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Le transport de magma dans des filons est traite dans deux situations geodynamiques. La premiere concerne l'ascension verticale de magma au travers de la lithosphere. Elle est traitee dans un espace a deux dimensions. L'ecoulement du fluide visqueux est envisage au travers de deux plaques elastiques, dont la hauteur delimite la distance entre la surface terrestre et le reservoir de magma. Il est montre que l'ascension est conditionnee par l'initiation des filons dans la lithosphere. La montee de magma est caracteristique de trois phases successives marquees par une vitesse quasi constante, une
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Pommier, Anne. "Propriétés électriques des magmas." Phd thesis, Université d'Orléans, 2009. http://tel.archives-ouvertes.fr/tel-00545608.

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Les expériences ont été menées pour déterminer les propriétés électriques des verres et liquides silicatés du Vésuve et du Kilauea par spectroscopie d'impédance. Une étude méthodologique des mesures à deux et quatre électrodes a amélioré la qualité des mesures électriques. Les mesures ont été faites entre 400 et 1400°C, 0.1 et 400MPa et pour des fugacités en oxygène de 10-8 à 0.2 bar. La conductivité électrique croît avec la température, les teneurs en eau et sodium et lorsque pression et fO2 diminuent. Des lois d'Arrhénius ont été déterminées dans les verres et liquides pour étudier les propr
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Reiners, Peter William. "Reactive melt transport in the mantle and petrogenesis of Hawaiian post-erosional magmas /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/6714.

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Le, Roux Véronique. "Interactions magma-roche et déformation en présence de magmas dans les péridotites de Lherz : implications pour l'évolution structurale, chimique et isotopique du manteau lithosphérique." Montpellier 2, 2008. http://www.theses.fr/2008MON20113.

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Dufils, Thomas. "Etude des propriétés physico-chimiques des magmas hydratés par dynamique moléculaire." Thesis, Paris 6, 2017. http://www.theses.fr/2017PA066240/document.

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Dans ce manuscrit, nous nous sommes intéressés aux propriétés des magmas ainsi qu’aux effets de l’eau sur celles-ci en utilisant la dynamique moléculaire classique. Après avoir mis en avant l’importance de l’eau dans les phénomènes géologiques et présenté quelques bases de dynamique moléculaire, nous présentons un champ de force pour les liquides silicatés anhydres. Nous utilisons ce champ de force pour étudier l’équation d’état, la structure et les propriétés de transport (viscosité, conductivité électrique, coefficient de diffusion) de liquides silicatés de composition aussi bien terrestre q
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Daniels, Katherine Anne. "Modelling magma transport : a study of dyke injection." Thesis, University of Bristol, 2013. http://hdl.handle.net/1983/b32d1ddc-a0ae-437e-8d7c-11d08c2cc72f.

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Dyke injection transports large volumes of magma over great distances, controlling the supply of magma to volcanoes and effectively releasing tensional stress at divergent plate margins. This thesis aims to improve understanding of dyke injection processes on different scales. Dyke shapes measured on the Isle of Rum have been analysed and show a mismatch between the currently accepted theory used to describe their shape, and the measured data. The measured dykes show wider edges than expected, consistent with wedging and cooling of magma in the dyke tips; wedged dykes can act as conduits for l
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Magde, Laura Suzan. "Mantle upwelling, melt generation, and magma transport beneath mid-ocean ridges." Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/55052.

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Menand, Thierry. "Transport de magma par fracturation hydraulique a travers la lithosphere terrestre." Paris 7, 2000. http://www.theses.fr/2000PA077153.

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Cette these etudie les conditions necessaires pour initier et propager un groupe de fissures remplies de liquide depuis un reservoir en surpression constante. Nous avons realise trois experiences de laboratoire differentes en utilisant de la gelatine pour simuler le comportement elastique cassant de la croute terrestre. Nous avons tout d'abord etudie l'initiation d'un groupe de fissures. Une couche de liquide est placee sous une couche de gelatine elastique cassante dans laquelle ont ete creees des fissures identiques, paralleles et regulierement espacees. Dans une premiere serie d'experiences
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Pinel, Virginie. "Transport et stockage de magma: suivi par interférométrie radar satellitaire et modélisation." Habilitation à diriger des recherches, Université de Grenoble, 2012. http://tel.archives-ouvertes.fr/tel-00840823.

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Dans une perspective de gestion de l'aléa volcanique, il est essentiel d'être capable de détecter, suffisamment tôt, un apport superficiel de magma et sa migration éventuelle vers la surface. Il est ensuite important de pouvoir prévoir la localisation de l'éruption à venir, son amplitude et le risque de déstabilisation de l'édifice volcanique associé. Dans ce manuscrit, je mets en perspective mes travaux de recherche qui concernent, à la fois, le suivi spatio-temporel de la migration du magma par mesure radar satellitaire et le développement de modèles mécaniques dynamiques prenant en compte l
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Robertson, Elspeth Annabel May. "Magma storage and transport at Kenyan Rift volcanoes : a remote sensing perspective." Thesis, University of Bristol, 2015. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.683731.

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The timescale and process of magma storage and transportation at continental rifts is not well understood. Extension, fault structures and hydrothermal systems all influence magma storage, volcano deformation and volatile emissions at rift volcanoes. This thesis uses a multidisciplinary approach to study these processes within the Kenyan Rift (KR), combining satellite and ground-based observations of deformation, structure and degassing. Using satellite radar (InSAR) , I show diverse deformation histories exhibited by 5 deforming volcanoes, including: coupled magmatic uplift-hydrothermal subsi
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Books on the topic "Transport de magmas"

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Wright, Thomas L. Two hundred years of magma transport and storage at Kīlauea Volcano, Hawaiʻi, 1790-2008. U.S. Geological Survey, 2014.

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1943-, Ryan Michael P., and Symposium on Magma Transport and Storage from Source to Eruption Site (1989 : Washington, D.C.), eds. Magma transport and storage. Wiley, 1990.

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Burchardt, Steffi. Volcanic and Igneous Plumbing Systems: Understanding Magma Transport, Storage, and Evolution in the Earth's Crust. Elsevier Science & Technology Books, 2018.

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Commercial Vehicles 2019. VDI Verlag, 2019. http://dx.doi.org/10.51202/9783181023501.

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Dieser VDI-Bericht ist ausschließlich als PDF-Datei erschienen! Sie möchten gerne erfahren, welche Themen auf der 15. Internationalen Konferenz in Baden-Baden präsentiert wurden? Dann schauen Sie sich das hier mal an: Content Plenary Lectures Electric buses in Cologne – Present state and perspective of KVB’s electric buses – Our plan for the complete transition of the bus fleet 1 J. Schwarze, Kölner Verkehrs-Betriebe AG, Cologne Vehicle Concepts The Mercedes-Benz eCitaro – A modular concept for sustainable electro mobility in city bus operations 9 D. Vorgerd, EvoBus GmbH, Mannheim The new MAN
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Balcerzak, Adam P., and Ilona Pietryka, eds. 11th International Conference on Applied Economics Contemporary Issues in Economy. Institute of Economic Research, 2021. http://dx.doi.org/10.24136/eep.abs.2021.1.

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The book contains abstracts submitted to 11th International Conference on Applied Economics Contemporary Issues in Economy, Poland 17-18 June 2021. The conference was organized by Institute of Economic Research (Poland), Polish Economic Society Branch in Toruń (Poland), Faculty of Economic Sciences, University of Warmia and Mazury in Olsztyn (Poland) in partnership with: Brno University of Technology (Czech Republic), “Constantin Brancusi” University of Targu-Jiu, Center of Fundamental and Applied Economic Studies (Romania), Lobachevsky State University of Nizhni Novgorod, Institute of Economi
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Book chapters on the topic "Transport de magmas"

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Frost, B. Ronald, Carol D. Frost, and Jacques L. R. Touret. "Magmas as a Source of Heat and Fluids in Granulite Metamorphism." In Fluid Movements — Element Transport and the Composition of the Deep Crust. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_1.

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Nutman, A. P., and A. A. Garde. "Fluid Control on Emplacement of Sialic Magmas During Archaean Crustal Accretion." In Fluid Movements — Element Transport and the Composition of the Deep Crust. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_21.

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Koyaguchi, Takehiro. "Dynamics of Mixing between Mafic and Silicic Magmas: Evidence from Volcanic Rocks." In Dynamic Processes of Material Transport and Transformation in the Earth’s Interior. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-3314-2_20.

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Fowler, Andrew. "Magma Transport." In Interdisciplinary Applied Mathematics. Springer London, 2011. http://dx.doi.org/10.1007/978-0-85729-721-1_9.

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Fernández, Carlos, Antonio Castro, J. D. De La Rosa, and I. Moreno-Ventas. "Rheological Aspects of Magma Transport Inferred from Rock Structures." In Petrology and Structural Geology. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-017-1717-5_5.

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Alt-Epping, Peter, and Larryn W. Diamond. "Reactive Transport and Numerical Modeling of Seafloor Hydrothermal Systems: A Review." In Magma to Microbe: Modeling Hydrothermal Processes at Ocean Spreading Centers. American Geophysical Union, 2013. http://dx.doi.org/10.1029/178gm09.

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Fowler, A. C. "Theories of Mushy Zones: Applications to Alloy Solidification, Magma Transport, Frost Heave and Igneous Intrusions." In Structure and Dynamics of Partially Solidified Systems. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3587-7_11.

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Nicholls, J. "CHAPTER 4. THE MATHEMATICS OF FLUID FLOW AND A SIMPLE APPLICATION TO PROBLEMS OF MAGMA TRANSPORT." In Modern Methods of Igneous Petrology, edited by James NICHOLLS and Kelly Russell. De Gruyter, 1990. http://dx.doi.org/10.1515/9781501508769-008.

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Magee, Craig, Richard E. Ernst, James Muirhead, Thomas Phillips, and Christopher A. L. Jackson. "Magma Transport Pathways in Large Igneous Provinces: Lessons from Combining Field Observations and Seismic Reflection Data." In Springer Geology. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-1666-1_2.

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Sato, Hiroki, Kenichi Muro, and Akira Hasegawa. "Three-dimensional Mapping of Magma Source and Transport Regions from Seismic Data: The Mantle Wedge beneath Northeastern Japan." In Q of the Earth: Global, Regional, and Laboratory Studies. Birkhäuser Basel, 1998. http://dx.doi.org/10.1007/978-3-0348-8711-3_7.

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Conference papers on the topic "Transport de magmas"

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Withjack, Martha O., and LeeAnn Srogi. "LATERAL TRANSPORT OF CAMP-RELATED MAGMAS BENEATH THE EASTERN NORTH AMERICAN RIFT SYSTEM AND MARGIN." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355723.

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Morris, Rebecca, and Dante Canil. "CO2 TRANSPORT IN ARC MAGMAS: EVIDENCE FROM UNIQUE ORBICULAR DIKES IN THE JURASSIC BONANZA ARC, VANCOUVER ISLAND, CANADA." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363011.

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Karlstrom, Leif, Scott R. Paterson, and A. Mark Jellinek. "A REVERSE ENERGY CASCADE FOR CRUSTAL MAGMA TRANSPORT." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298728.

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Aasman, Jordan, Linda Valerio, Jesse Batko, and Beth Klein. "MAGIS-100 Laser Transport Vacuum Simulations and LED Atom Tracker." In MAGIS-100 Laser Transport Vacuum Simulations and LED Atom Tracker. US DOE, 2020. http://dx.doi.org/10.2172/1778681.

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Peter, Geoffrey J. "Application of Coupled Thermo-Hydro-Mechanical-Chemical (THMC) Processes in Hydrothermal Systems to Processes Near a High-Level Nuclear Waste Repository." In ASME 2011 14th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2011. http://dx.doi.org/10.1115/icem2011-59246.

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Modeling of coupled processes in the geology near a high-level nuclear waste repository is similar to the modeling of coupled Thermo-Hydro-Mechanical-Chemical (THMC) processes that occur in magma-hydrothermal systems. Former Professor Denis Norton and his colleagues at the Geoscience Department at University of Arizona studied magma-hydrothermal systems extensively. These hydro-thermal codes were verified by obtaining excellent matches between calculated δ18O–values and measured δ18O–values in three principal rock units: basalt, gabbro, and gneiss. This paper reviews the concept of transport t
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Balta, J. Brian. "IMPACT OF THE MARTIAN LITHOSPHERE ON MANTLE MELTING AND MAGMA TRANSPORT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285886.

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Chen, Kewei, Hongbin Zhan, Erick Burns, Steven E. Ingebritsen, and Pierre Agrinier. "THE INFLUENCE OF EPISODIC SHALLOW MAGMA DEGASSING ON HEAT AND CHEMICAL TRANSPORT IN VOLCANIC HYDROTHERMAL SYSTEMS." In 115th Annual GSA Cordilleran Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019cd-329518.

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Itoh, Akitoshi, Masahiro Kawamata, and Tomohiro Hirai. "An Object Transportation System Using Controlled Daphnia Magna." In ASME 2012 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/imece2012-87338.

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In this study, we tried to create an object transportation system using Daphnia magna. We developed a target object for the transportation experiment using a 5-mm-diameter transparent acrylic rod with a hole in the lower part. Black film and a small white ball were attached to the top surface of the object in order to improve contrast and allow easier position detection during image processing. The daphnia were first directed to the guide point, about 10 mm opposite the desired transportation direction. They were then guided to collide with the object. If a collision did not occur, they were g
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Buongiorno, J. "A Non-Homogeneous Equilibrium Model for Convective Transport in Flowing Nanofluids." In ASME 2005 Summer Heat Transfer Conference collocated with the ASME 2005 Pacific Rim Technical Conference and Exhibition on Integration and Packaging of MEMS, NEMS, and Electronic Systems. ASMEDC, 2005. http://dx.doi.org/10.1115/ht2005-72072.

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A base fluid (e.g., water, ethanol, oil) in which nano-sized (1–100 nm) particles of a different material are dispersed, is known as a nanofluid. Nanofluids are attractive because the presence of the nanoparticles enhances energy transport considerably. As a result, nanofluids have higher thermal conductivity and single-phase heat transfer coefficients than their base fluids. In particular, the heat transfer coefficient increases appear to go beyond the mere thermal-conductivity effect, and cannot be predicted by traditional pure-fluid correlations such as Dittus-Boelter’s. In the nanofluid li
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Rice, A., A. Botha, K. Harrison, et al. "3-Dimensional Calculations Of Transport Processes Associated With Convection In Freezing Magma Chambers And Attendant Hydrothermal Circulation In Country Rock." In 5th SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.223.020.

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Reports on the topic "Transport de magmas"

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Phillips, Benjamin R., W. Scott Baldridge, Carl W. Gable, and James M. Sicilian. Duration of the Banco Bonito Rhyolite Eruption, Vales Caldera, New Mexico based on magma transport modeling. Office of Scientific and Technical Information (OSTI), 2007. http://dx.doi.org/10.2172/1237263.

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