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Dissertations / Theses on the topic 'Basaloid'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

Pereira, Carlos Henrique. "Expressão de proteínas de adesão (e-caderina e β - catenina) e proliferação celular (ki-67) no fronte de invasão tumoral de Carcinomas Espinocelular e Escamoso Basalóide". Universidade Federal de Goiás, 2014. http://repositorio.bc.ufg.br/tede/handle/tede/5158.

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Submitted by Luciana Ferreira (lucgeral@gmail.com) on 2016-01-29T08:31:16Z No. of bitstreams: 2 Dissertação - Carlos Henrique Pereira - 2014.pdf: 3850945 bytes, checksum: 985b041e7a863070b3fa0562180a40f3 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5)<br>Approved for entry into archive by Luciana Ferreira (lucgeral@gmail.com) on 2016-01-29T08:33:08Z (GMT) No. of bitstreams: 2 Dissertação - Carlos Henrique Pereira - 2014.pdf: 3850945 bytes, checksum: 985b041e7a863070b3fa0562180a40f3 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5)

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2

Lam, Alfred. "Molecular Pathology of Oesophageal Tumours." Thesis, Griffith University, 2006. http://hdl.handle.net/10072/365187.

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Oesophageal tumours are very common worldwide. This thesis aims to delineate the clinicopathological features and molecular biology of oesophageal tumours in Hong Kong Chinese. Over a 30-year study period, oesophageal tumours were obtained in the pathology files of the Queen Mary Hospital, Hong Kong. The tumours were prevalent in males and had a modal peak occurrence in the 7th decade. Patients often presented at an advanced stages. At autopsy, the prevalence of incidental oesophageal cancers and early-stage cancers were low. Many histological subtypes of oesophageal cancers were noted and wer

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3

Ayx, Isabelle Jessica Veronika [Verfasser], Henning [Akademischer Betreuer] Bier, and Thomas [Akademischer Betreuer] Stark. "Vergleichende Analyse des Angiogenese- und Metastasierungsverhaltens basaloid-squamöser Plattenepithelkarzinome gegenüber herkömmlichen Plattenepithelkarzinomen des Kopf-Hals-Bereichs / Isabelle Jessica Veronika Ayx. Gutachter: Thomas Stark ; Henning August Bier. Betreuer: Henning August Bier." München : Universitätsbibliothek der TU München, 2014. http://d-nb.info/1050025709/34.

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4

Witham, Fred. "The degassing of basaltic magma chambers." Thesis, University of Bristol, 2008. http://hdl.handle.net/1983/290a02f5-ab6b-4a62-8cd9-e328bed2434f.

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I present an integrated study of volcanic degassing processes coupled with the impact of degassing on magma chamber dynamics. A one-dimensional model of heat flow inside an incipient magma reservoir is derived by considering the thermal effect of repeated basaltic sill intrusions into the crust. The minimum magma flux required to maintain melt indefinitely, i.e. to form a ‘magma chamber’, is found as a function of intrusion depth. Despite the time-dependent nature of the modelled solutions, fluxes can be approximated by a steady state solution when cooling is dominated by heat loss through the

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5

COSTA, Michela. "Bromine degassing in basaltic volcanic systems." Doctoral thesis, Università degli Studi di Palermo, 2014. http://hdl.handle.net/10447/91244.

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6

Guilbaud, Marie-NoeÌˆlle. "The origin of basaltic lava flow textures." Thesis, Open University, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.429548.

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7

Brito, Jorge Manuel Santos Sousa. "Phosphates in suspensions of alkaline, basaltic soils." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185198.

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The phosphate solid-solution activities in the A and A₁ horizons of ten alkaline soils from basalt were calculated in order to assess their conformity to solid-solution behavior. Nine soils were from the Cape Verde Islands and one from Arizona. Four of the Cape Verdean soils belonged to the same series (Ponta) but presented different levels of P fertilization. The other soils were not fertilized. All soils behaved in conformity with solid-solution theory. Three assumptions were made: (1) Surfaces of minerals are similar because of weathering; (2) Partial equilibrium was reached; (3) The mole f

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8

Armshaw, Derek. "Garnet- and clinopyroxene-liquid equilibria at high pressure : an experimental study in part of the system CaO-MgO-FeO-Al₂O₃-SiO₂ with relevance to garnet-lherzolites." Thesis, University of Edinburgh, 1987. http://hdl.handle.net/1842/11387.

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9

Bell, Andrew Forbes. "Patterns of volcano-tectonic seismicity at basaltic volcanoes." Thesis, University College London (University of London), 2008. http://discovery.ucl.ac.uk/1444163/.

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Accelerating rates of volcano-tectonic (VT) earthquakes are a common precursor to volcanic eruptions and reflect fracture growth within the edifice. Theoretical models interpret the patterns in terms of failure of the volcanic edifice under the magmatic load and promise improved eruption forecasting. However, many eruptions at frequently active basaltic volcanoes are reported to begin with little change in the rate of VT earthquakes, apparently in conflict with edifice failure models. This thesis investigates the spatial and temporal patterns of VT earthquakes associated with eruptive and intr

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10

Dalpé, Claude. "Trace element partitioning between amphibole and basaltic melt." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0007/NQ44399.pdf.

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11

Dalpé, Claude. "Trace element partitioning between amphibole and basaltic melt." Thesis, McGill University, 1997. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=34939.

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The effects of composition, pressure and oxygen fugacity on partition coefficients between amphibole and hydrous basaltic melt were studied at 1.5 to 2.5 GPa and 1000 to 1130°C. Partition coefficients (D i = concentration of element i in amphibole/concentration of i in melt) of large-ion-lithophile elements (LILE: Rb, Sr, Ba), high-field-strength elements (HFSE: Y, Zr, Nb, Ta, Hf), and rare-earth elements (REE: La to Lu) were determined between amphiboles and coexisting quenched melts created by partial crystallization of seven different starting compositions in a piston-cylinder high-pressure

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12

Sigfússon, Bergur. "Reactive transport of arsenic through basaltic porous media." Thesis, University of Aberdeen, 2009. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=103575.

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This thesis studied the volcanic and geothermal source of arsenic (As) and its fate in shallow ground waters and upon entering the ocean by means of experimental and field measurements combined with geochemical modeling. Arsenic enters the atmosphere and hydrosphere from degassing magmas and during volcanic eruptions. The November 2004 eruption within the Vatnajökull Glacier, Iceland, provided an opportunity to study elemental fluxes from volcanic eruptions into the environment. According to geochemical modeling, lowering of pH due to magma gases during the eruption led to rapid tephra dissolu

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13

Jones, Thomas James. "Fissures and fountains : magma dynamics in basaltic conduits." Thesis, Durham University, 2018. http://etheses.dur.ac.uk/12688/.

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Basaltic volcanoes are responsible for the bulk of the planet’s magma output. Their eruptions are often spectacular and can have serious impacts on a local scale (through lava flows) and regional scale (through emission of ash and toxic gases). However, hazard planning and mitigation is challenging because these eruptions can be highly variable both temporally, lasting from hours to months, and spatially, localizing from a long, linear fissure to a discrete vent. In this thesis, I will explore the role that magma transport and eruption dynamics play in controlling the evolution of basaltic fis

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14

Pering, Tom D. "Bubbles in basalts : measuring and modelling basaltic degassing." Thesis, University of Sheffield, 2015. http://etheses.whiterose.ac.uk/12528/.

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Basaltic degassing is driven by the release of CO2, H2O, and SO2. Hitherto, the measurement of SO2 has been commonplace due to the lack of significant ambient atmospheric content. UV camera technology is currently among the best of techniques to measure this SO2 release from volcanoes given its high spatial and temporal resolutions. Given that an elevated CO2 flux can be an indication of magma movement at depth, a reliable method of measuring this species at similarly high temporal resolutions would be valuable. A technique making this possible is described here. This technique combines measur

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15

Knox, Dayan. "Nucleus basalis cholinergic lesions and defense responses." Connect to resource, 2005. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1127235519.

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Thesis (Ph. D.)--Ohio State University, 2005.<br>Title from first page of PDF file. Document formatted into pages; contains xii, 103 p.; also includes graphics (some col.). Includes bibliographical references (p. 90-103). Available online via OhioLINK's ETD Center

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Knox, Dayan K. "Nucleus basalis cholinergic lesions and defense responses." The Ohio State University, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=osu1127235519.

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17

Woodell, Daniel Robert. "Constraints on formation of columnar joints in basaltic lava." Thesis, University of British Columbia, 2012. http://hdl.handle.net/2429/43777.

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Columnar joints form as a brittle relaxation response to tensile stresses within cooling lava flows and magma bodies, and are found in lavas that vary greatly in chemistry and outcrop geometry. However, columnar joints do not form in all cooling igneous rocks, and the specific conditions under which columnar joints form are unknown. In this study, outcrops containing columns in the Cheakamus Valley basalt flows near Whistler, BC are studied, and the size, orientation, and distribution of columns is recorded. Forward numerical models using the finite element method are created with Matlab us

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18

James, Sarah Louise. "The geochemistry of secondary zeolites from tertiary basaltic terrains." Thesis, Royal Holloway, University of London, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.325118.

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19

McAlister, John J. "Characterisation of basaltic weathering products by modern analytical techniques." Thesis, Queen's University Belfast, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.329424.

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20

Li, Yuyu M. S. "Petrologic Insights into Basaltic Magma Genesis beneath East Antarctica." Bowling Green State University / OhioLINK, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1593363487482443.

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21

Fuenkajorn, Kittitep. "EXPERIMENTAL ASSESSMENT OF BOREHOLE DRILLING DAMAGE IN BASALTIC ROCKS." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/291691.

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22

Martyn, Kendal Roger. "The relationship between the geochemistry of spinel peridotite nodules and alkali basalt." Thesis, University of Cambridge, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.340974.

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23

Banks, Joanna Mary. "Nucleation of magma-driven fractures in the asthenospheric mantle." Thesis, University of Liverpool, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.309901.

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24

Salem, Lois Claire. "Magmatic processes at basaltic volcanoes : insights from the crystal cargo." Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/277726.

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A plethora of magmatic processing occurs in magma reservoirs, where melts are stored prior to eruption. Magma reservoirs are complex, open systems, and often multiple reservoirs are partially inter-connected from source to surface, giving rise to the term 'volcanic plumbing system'. Parental melts feeding these reservoirs can have diverse and distinct geochemical and petrological characteristics, and be variably evolved or enriched. These melts can also bring with them a crystal cargo that may remain in equilibrium in the magma reservoir, but may also be modified by reaction, resorption, cryst

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25

Tarragó, Aymerich Mariona. "Modelization of the vitrification of sewage sludge using a basaltic matrix." Doctoral thesis, Universitat de Barcelona, 2018. http://hdl.handle.net/10803/668461.

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Sewage sludge is a high volume, potentially toxic waste generated during the decontamination process of wastewater. Improved solutions for waste disposal require its conversion into an end product or at least a raw material for new applications. The chemical composition of sewage is similar to that of a basalt enriched in P and Ca, hence it may be inertized by vitrification. The experimental strategy is based on producing glasses from mixtures containing basalt, P and/or Ca to study the production of glass from sewage sludge. Selected glass compositions are then doped with toxic elements (Ba,

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26

Duygulu, Yusuf Bahadir. "Decolorization Of Synthetic Dye Solutions By Using Basaltic Tephra And Clinoptilolite." Master's thesis, METU, 2004. http://etd.lib.metu.edu.tr/upload/12605241/index.pdf.

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Discharge of colored effluents without decoloration originated from textile industries may cause serious problems in the receiving environments. In this study, natural materials that are basaltic tephra and clinoptilolite were used to remove various dyestuffs used in the textile industry. Those materials are cheap and available in large quantities in Turkey. The investigation of adsorption of basic, acidic and reactive dyes on these materials is the objective of this study. During preliminary experiments it was seen that adsorption equilibrium was reached in about 2 days. In adsorption ex

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27

Beckett, F. M. "Exchange flow experiments and implications for degasing processes at basaltic volcanoes." Thesis, University of Bristol, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.573419.

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Persistently active basaltic volcanoes are characterised by Strombolian eruptions that punctuate continuous passive degassing. Persistent passive degassing can be driven by an exchange flow of magma within the conduit. To interpret persistent gas emissions and changes in activity requires some knowledge of the flow regime and an understanding of how its volume flux depends on the physical properties of the magma and the conduit geometry. This thesis presents an experimental study of buoyancy-driven, low Reynolds number, (Re < 6) exchange flow of two Newtonian fluids in a vertical cylindrical p

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28

Collins, S. J. "Degassing of volatiles and semi-volatile trace elements at basaltic volcanoes." Thesis, University of Cambridge, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.597860.

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At Mt. Etna, Italy, vigorous gas-rich eruptions in 2001, 2002 and 2003 were followed by gas-poor eruptions in 2004, 2006 and 2007. Contrary to expectation, melt inclusion compositions indicate that magmas erupted between 2004 to 2007 did not follow similar degassing paths as recorded in 2001 and 2002 and that are expected from the solubility laws of CO<sub>2</sub> and H<sub>2</sub>O. Instead melts stored in the plumbing system since 2002 reequilibrated with CO<sub>2</sub>-rich gases from depth. Sustained gas percolation caused loss of water and enhancement of CO<sub>2</sub> in the evolving mel

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29

Johnson, Emily Renee. "Volatiles in basaltic magmas from central Mexico : from subduction to eruption /." Thesis, Connect to title online (Scholars' Bank) Connect to title online (ProQuest), 2008. http://hdl.handle.net/1794/8331.

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Thesis (Ph. D.)--University of Oregon, 2008.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 153-167). Also available online in Scholars' Bank; and in ProQuest, free to University of Oregon users.

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30

Reynolds, Peter William. "Monogenetic basaltic edifices : their architecture, volcanology and importance in hydrocarbon basins." Thesis, Durham University, 2015. http://etheses.dur.ac.uk/11369/.

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Flood basalt provinces host significant hydrocarbon reserves. The provinces are produced during fissure eruptions which construct volcanic edifices atop an erupting dyke. The edifices are important components of volcanic-affected hydrocarbon basins; they provide insights into the underlying structural and magmatic plumbing systems, as well as acting as fluid migration pathways after burial. Furthermore, the edifices host a wealth of volcanological evidence that can be used to derive information relating to eruption dynamics such as eruption column height, mass flux and duration; as well as pro

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31

Sant, Christopher Joseph. "Geothermal Alteration of Basaltic Core from the Snake River Plain, Idaho." DigitalCommons@USU, 2012. https://digitalcommons.usu.edu/etd/1451.

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The Snake River Plain is located in the southern part of the state of Idaho. The eastern plain, on which this study focuses, is a trail of volcanics from the Yellowstone hotspot. Three exploratory geothermal wells were drilled on the Snake River Plain. This project analyzes basaltic core from the first well at Kimama, north of Burley, Idaho. The objectives of this project are to establish zones of geothermal alteration and analyze the potential for geothermal power production using sub-aquifer resources on the axial volcanic zone of the Snake River Plain. Thirty samples from 1,912 m of core we

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32

Brehaut, Janet Catherine. "2D-Modelling of Earthquake-Induced Rockfall from Basaltic Ignimbrite Cliffs at Redcliffs, Christchurch, New Zealand." Thesis, University of Canterbury. Geological Sciences, 2012. http://hdl.handle.net/10092/9172.

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This thesis is concerned with modelling rockfall parameters associated with cliff collapse debris and the resultant “ramp” that formed following the high peak ground acceleration (PGA) events of 22 February 2011 and 13 June 2011. The Christchurch suburb of Redcliffs, located at the base of the Port Hills on the northern side of Banks Peninsula, New Zealand, is comprised of Miocene-age volcanics with valley-floor infilling marine sediments. The area is dominated by basaltic lava flows of the Mt Pleasant Formation, which is a suite of rocks forming part of the Lyttelton Volcanic Group that were

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33

Mathieson, Gillian Ann. "Olivine-basaltic melt re-equilibration rates and their implications for crystallisation processes." Thesis, University of Sheffield, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.343508.

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34

Soule, Samuel Adam. "Basaltic lava flow surface morphology : genesis, evolution, and impact on flow dynamics /." view abstract or download file of text, 2003. http://wwwlib.umi.com/cr/uoregon/fullcit?p3102190.

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Thesis (Ph. D.)--University of Oregon, 2003.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 271-279). Also available for download via the World Wide Web; free to University of Oregon users.

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35

Allen, Daniel R. "Temperature and Variability of Three Ionian Volcanoes." BYU ScholarsArchive, 2010. https://scholarsarchive.byu.edu/etd/2591.

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Cassini spacecraft images of Io obtained during its flyby of Jupiter in late 2000 and early 2001 were used to determine the lava composition and eruption style of three faint hotspots, Pillan, Wayland, and Loki. We found a maximum color temperature of 1130+/-289 K for Pillan and maximum color temperatures of 1297+/-289 K and 1387+/-287 K for Wayland and Loki, respectively. These temperatures are suggestive of basaltic lava. The temperatures with the best signal-to-noise ratios also suggested basaltic lava and were found to be 780+/-189 K, 1116+/-250 K, and 1017+/-177 K for Pillan, Wayland, and

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36

Pohlmann, Michael, Katerina Dontsova, Robert Root, Joaquin Ruiz, Peter Troch, and Jon Chorover. "Pore water chemistry reveals gradients in mineral transformation across a model basaltic hillslope." AMER GEOPHYSICAL UNION, 2016. http://hdl.handle.net/10150/621416.

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The extent of weathering incongruency during soil formation from rock controls local carbon and nutrient cycling in ecosystems, as well as the evolution of hydrologic flow paths. Prior studies of basalt weathering, including those that have quantified the dynamics of well-mixed, bench-scale laboratory reactors or characterized the structure and integrated response of field systems, indicate a strong influence of system scale on weathering rate and trajectory. For example, integrated catchment response tends to produce lower weathering rates than do well mixed reactors, but the mechanisms under

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37

Liu, Emma J. "The generation of volcanic ash during basaltic hydromagmatic eruptions : from fragmentation to resuspension." Thesis, University of Bristol, 2016. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.702943.

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Explosive magma-water interaction (MWI) during hydromagmatic eruptions generates substantially more fine-grained volcanic ash than equivalent 'dry' eruptions. However, the social and economic disruption caused by recent subglacial eruptions in Iceland highlighted gaps in our knowledge of the mechanisms responsible for fine fragmentation during MWI and the resulting implications for modelling ash dispersion. By developing new ways to characterise and interpret volcanic ash properties, this thesis shows that (a) magmatic vesiculation prior to MWI is the rule rather than the exception, (b) rapid

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38

Arendt, Thomas, Martina K. Brückner, Markus Morawski, Carsten Jäger, and Hermann-Josef Gertz. "Early neurone loss in Alzheimer’s disease." Universitätsbibliothek Leipzig, 2015. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-160935.

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Alzheimer’s disease (AD) is a degenerative disorder where the distribution of pathology throughout the brain is not random but follows a predictive pattern used for pathological staging. While the involvement of defined functional systems is fairly well established for more advanced stages, the initial sites of degeneration are still ill defined. The prevailing concept suggests an origin within the transentorhinal and entorhinal cortex (EC) from where pathology spreads to other areas. Still, this concept has been challenged recently suggesting a potential origin of degeneration in nonthalamic

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39

Findlay, Jonathan. "Petrology, geochemistry and evolution of the Labrador Trough Basaltic Suite, Labrador and New Quebec." Thesis, University of Ottawa (Canada), 1996. http://hdl.handle.net/10393/9934.

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The central Labrador Trough is an Early Proterozoic volcano-sedimentary succession which preserves the remnants of a major magmatic province, the Labrador Trough Basaltic Suite (LTBS). The Menihek gabbros, which are distinctive members of the LTBS, form a sill-sediment complex with turbidites of the Menihek Formation. The Menihek gabbros often exhibit spectacular plagioclase glomeroporphyritic textures. Tholeiitic basalts of the LTBS (Le Fer and upper Menihek/Willbob basalts) exhibit many textural and geochemical similarities, despite a difference of $\sim$260 Ma in the ages of the two princip

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40

Guernina, Souad. "An experimental study of the effect of Fe-Ti oxide crystallization on basaltic liquids." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1996. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp04/MQ37124.pdf.

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41

Léveillé, Richard John. "Biogeochemistry of carbonate-silicate deposits associated with microbial mats in basaltic caves, Kauai, Hawaii." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ58402.pdf.

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42

Morgavi, Daniele [Verfasser], and Donald Bruce [Akademischer Betreuer] Dingwell. "Magma mixing : interaction between rhyolitic and basaltic melt / Daniele Morgavi. Betreuer: Donald Bruce Dingwell." München : Universitätsbibliothek der Ludwig-Maximilians-Universität, 2014. http://d-nb.info/1047543494/34.

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43

Suckale, Jenny. "Direct numerical simulations of multiphase flow with applications to basaltic volcanism and planetary evolution." Thesis, Massachusetts Institute of Technology, 2011. http://hdl.handle.net/1721.1/68889.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2011.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 243-266).<br>Multiphase flows are an essential component of natural systems: They affect the explosivity of volcanic eruptions, shape the landscape of terrestrial planets, and govern subsurface flow in hydrocarbon reservoirs. Advancing our fundamental understanding and predictive capabilities of multiphase flows is a problem of immense importance for both industrial and scientific purposes. This th

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44

Mitchell, Clive J. "Petrology and geochemistry of basaltic rocks of the Falkland Islands and Deccan Traps (India)." Thesis, University of Oxford, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.670335.

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45

Field, Scott A. "Patch exploitation and defence in the egg parasitoid Trissolcus basalis Wollaston (Hymenoptera : Scelionidae)." Title page, contents and summary only, 1997. http://web4.library.adelaide.edu.au/theses/09PH/09phf456.pdf.

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Bibliography: leaves 175-191. Trissolcus basalis (Wollaston) is a solitary endoparasitoid of the eggs of many pentatomid bugs. It is a quasi-gregarious scelenoid and aggressively defends host patches. In the Adelaide (S. Aust.) region its most abundant host is the native horehound bug, Agonoscelis rutila (Fabricius). This study of patch defence draws together important areas of research in parasitoid behavioural ecology, including the theories of adaptive superparasitism, sex ratio decisions, foraging behaviour and contest resolution.

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46

Poustovetov, Alexei Anatolievich. "Numerical modeling of chemical equilibria between chromian spinel, olivine, and basaltic melt, with petrologic applications." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0016/NQ54428.pdf.

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47

Pérez, Fernández Wendy [Verfasser]. "Basaltic Plinian and violent Surtseyan eruptions from the Masaya Caldera Complex, Nicaragua / Wendy Pérez Fernández." Kiel : Universitätsbibliothek Kiel, 2008. http://d-nb.info/1019552913/34.

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48

Bondre, Ninad R. "FIELD AND GEOCHEMICAL INVESTIGATION OF BASALTIC MAGMATISM IN THE WESTERN UNITED STATES AND WESTERN INDIA." Miami University / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=miami1164916380.

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49

Radoman-Shaw, Brandon G. "Exposure of Basaltic Materials to Venus Surface Conditions using the Glenn Extreme Environment Rig (GEER)." Case Western Reserve University School of Graduate Studies / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=case1557312457308105.

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Serrano, Lina. "Jurassic magmatism in Patagonia, Mauritania and Mali: Examples of silicic and basaltic Large Igneous Provinces." Doctoral thesis, Università degli studi di Padova, 2014. http://hdl.handle.net/11577/3423851.

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Abstract:

At the end of the Triassic and during Jurassic times, the Central Atlantic Magmatic Province (CAMP) with a dominant mafic composition, and the mainly felsic Patagonian Province (PA) were formed in the context of Pangea break-up. CAMP basaltic to basaltic-andesitic dykes and sills from Hank and Hodh, in Mauritania, and Kaarta, in Mali, were emplaced at ca. 197 Ma yielding a signature defined by low to high TiO2-values (0.39 - 2.29 wt.%), Nb-Ta troughs, Pb spikes and enriched Nd-Sr-Pb compositions (143Nd/144Nd201Ma: 0.51224 - 0.51241, 87Sr/86Sr201Ma: 0.70572 - 0.70795, 207Pb/204Pb201Ma: 15.61 –

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