Relevant bibliographies by topics / Volcanisme effusif

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Volcanisme effusif'

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

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Journal articles on the topic "Volcanisme effusif"

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Kröchert, Jörg Buchner, Martin Schmieder, Holger Maurer, Marco Walter, Annette Strasser, and Marcel Strasser. "Effusive melilititic volcanism on the Swabian Alb the Sternberg volcano (Gomadingen)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 160, no. 4 (December 1, 2009): 315–23. http://dx.doi.org/10.1127/1860-1804/2009/0160-0315.

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Smellie, John L. "Chapter 1.2 Antarctic volcanism: volcanology and palaeoenvironmental overview." Geological Society, London, Memoirs 55, no. 1 (2021): 19–42. http://dx.doi.org/10.1144/m55-2020-1.

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AbstractSince Jurassic time (c.200 Ma), Antarctica has had a greater diversity of volcanism than other southern continents. It includes: (1) voluminous mafic and felsic volcanism associated with the break-up of Gondwana; (2) a long-lived continental margin volcanic arc, including back-arc alkaline volcanism linked to slab rollback; (3) small-volume mafic alkaline volcanism associated with slab-window formation; and (4) one of Earth's major continental rift zones, the West Antarctic Rift System (WARS), with its numerous large alkaline central volcanoes. Several of Antarctica's volcanoes are still active. This chapter is a review of the major volcanic episodes and their principal characteristics, in their tectonic, volcanological and palaeoenvironmental contexts. Jurassic Gondwana break-up was associated with large-scale volcanism that caused global environmental changes and associated mass extinctions. The volcanic arc was a major extensional arc characterized by alternating volcanic flare-ups and lulls. The Neogene rift-related alkaline volcanism is dominated by effusive glaciovolcanic eruptions, overwhelmingly as both pāhoehoe- and ‘a‘ā-sourced lava-fed deltas. The rift is conspicuously poor in pyroclastic rocks due to the advection and removal of tephra erupted during glacial intervals. Volcanological investigations of the Neogene volcanism have also significantly increased our knowledge of the critical parameters and development of the Antarctic Ice Sheet.
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DeWolfe, Y. M., H. L. Gibson, B. Lafrance, and A. H. Bailes. "Volcanic reconstruction of Paleoproterozoic arc volcanoes: the Hidden and Louis formations, Flin Flon, Manitoba, CanadaThis is a companion paper to DeWolfe, Y.M., Gibson, H.L., and Piercey, S.J. 2009. Petrogenesis of the 1.9 Ga mafic hanging wall sequence to the Flin Flon, Callinan, and Triple 7 massive sulphide deposits, Flin Flon, Manitoba, Canada. Canadian Journal of Earth Sciences, 46: this issue." Canadian Journal of Earth Sciences 46, no. 7 (July 2009): 481–508. http://dx.doi.org/10.1139/e09-031.

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The hanging wall to the Flin Flon, Callinan, and Triple 7 volcanogenic massive sulphide deposits of the Flin Flon district is composed of the Hidden and Louis formations. The contact between these formations is marked by mafic tuff that represents a hiatus in effusive volcanism. The formations form a composite volcanic edifice that was erupted and grew within a large, volcanic–tectonic subsidence structure (hosting the deposits) that developed within a rifted-arc environment. The formations are evidence of resurgent effusive volcanism and subsidence following a hiatus in volcanism marked by ore formation since they consist of dominantly basaltic flows, sills, and volcaniclastic rocks with subordinate basaltic andesite and rhyodacitic flows and volcaniclastic rocks. The Hidden formation is interpreted to represent a small shield volcano and the Louis formation a separate shield volcano that developed on its flank. Both the Hidden and Louis volcanic edifices were constructed by continuous, low-volume eruptions of pillow lava. A gradual change from a dominantly extensional environment during the formation of the footwall Flin Flon formation to a progressively more dominant convergent environment during the emplacement of the hanging wall suggests that the Hidden and Louis formations are unlikely to host significant volcanogenic massive sulphide-type mineralization. However, synvolcanic structures in the formations define structural corridors that project downwards into the footwall where they encompass massive sulphide mineralization, indicating their control on ore formation, longevity,and reactivation as magma and fluid pathways during the growth of the Hidden and Louis volcanoes.
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Inza, Coulibaly, Kouamelan Alain Nicaise, Djro Sagbrou Chérubin, and Coulibaly Yacouba. "Petrographie Des Volcanites Et Plutonites De La Partie Sud Du Sillon Volcano-Sedimentaire De Toumodi-Fetekro (Cote D’ivoire)." European Scientific Journal, ESJ 13, no. 30 (October 31, 2017): 199. http://dx.doi.org/10.19044/esj.2017.v13n30p199.

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The southern part of Toumodi-Fètêkro greenstone belt is located in the Center - Southeast of Ivory Coast. Petrographic study of volcanic and plutonic rocks shows three units. The first unit is composed of basaltic to rhyolitic lavas which imply effusive character. Then we have volcanosedimentary unit composed of pyroclastic formations (lapilli tuff, breccia, ash deposit and ignimbrites) and the pillow-lavas. Indeed, the presence of this last shows clearly that an explosive volcanism and a submarine effusive volcanism have occurred during during the setting of Toumodi-Fètêkro belt. Plutonic unit is constituted of gabbroic to granitic rocks. Sericite, chlorite, epidote observed in these rocks are consistent with the impacts of greenschist facies metamorphism. The rocks of the southern part of the Toumodi-Fètêkro greenstone belt are formed in a subduction context rather than in oceanic plateaus context because of the old inheritance, sometimes of Archean age, found somewhere in theBirimiandomain. The lithologies of the southern part of Toumodi-Fètêkro meet elsewhere in the other Birimian greenstone belts. Also, these lithologies are affected by a hydrothermal alteration due to the abundant veins of quartz, carbonates, sericite, chlorite, epidote, sulphides and oxides. However, volcanic show in some places amphibolit facies metamorphism.
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Filipovich, Ruben, Walter Báez, Emilce Bustos, Agustina Villagrán, Agostina Chiodi, and Jose Viramonte. "Estilos eruptivos asociados al volcanismo monogenético máfico de la región de Pasto Ventura, Puna Austral, Argentina." Andean Geology 46, no. 2 (May 31, 2019): 300. http://dx.doi.org/10.5027/andgeov46n2-3091.

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One of the most outstanding features of the Southern Puna is the occurrence of a widespread monogenetic mafic volcanism during Neogene-Quaternary. Despite a number of published papers focusing on the petrogenesis of this back-arc volcanism, works aimed on its physical volcanology are scarce. This paper presents the characterization of the monogenetic mafic volcanism in the Pasto Ventura region, located in the southeast edge of the Southern Puna. The results show that in the Pasto Ventura region there is a low density of small-volume eruptive centers aligned with regional tectonic structures and a significant variability in eruptive styles (effusive, strombolian, hawaiian, violent strombolian and phreatomagmatic) and typology of volcanic structures (domes, scoria cones, maars and tuff rings). The first of these features is explained by a limited magma flow rate from the deep source and the use of favorable tectonic structures (oriented obliquely to the regional maximum compression direction) for the ascent of small volumes of magma through the upper crust. The variability of eruptive styles responds to the complex interaction of different endogenous and exogenous factors. The occurrence of effusive or explosive eruptions depends on the differences in magma ascent rates including periods of stagnation in the upper crust, which in turn control the efficiency of degassing and ultimately the occurrence of fragmentation. On the other hand, the more humid local climatic conditions (~150 mm/year), which are related to the geographical position of the Pasto Ventura region in the eastern edge of the Puna, favor the occurrence of phreatomagmatic activity. Phreatomagmatic activity also varies according to the topography, substrate typology and depth at which water-magma interaction occurs.
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Mahoney, J. Brian, Richard M. Friedman, and Sean D. McKinley. "Evolution of a Middle Jurassic volcanic arc: stratigraphic, isotopic, and geochemical characteristics of the Harrison Lake Formation, southwestern British Columbia." Canadian Journal of Earth Sciences 32, no. 10 (October 1, 1995): 1759–76. http://dx.doi.org/10.1139/e95-137.

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The Harrison Lake Formation is an Early to Middle Jurassic volcanic-arc assemblage unconformably overlying Triassic oceanic basement in the eastern Coast Belt of southwestern British Columbia. The formation is subdivided into four members including, in ascending order, the Celia Cove Member (conglomerate), the Francis Lake Member (fine-grained strata), the Weaver Lake Member (flows and breccias), and the Echo Island Member (pyroclastic and epiclastic strata). New biostratigraphic constraints pinpoint the initiation of volcanism to late early Toarcian. U–Pb geochronology demonstrates the arc was active until at least late Bajocian–early Bathonian time (166.0 ± 0.4 Ma), and that the timing of arc volcanism strongly overlaps emplacement of both hypabyssal intrusions (Hemlock Valley stock) and deep-seated plutons (Mount Jasper pluton) within and adjacent to the arc. Geochemical data indicate the arc is of medium- to high-K calc-alkaline affinity, and is strongly light rare earth element enriched (LaN/YbN = 1.5 – 2.5). Nd and Sr isotopic data from primary volcanic rocks demonstrate the juvenile nature of the magmatic system, but isotopic data from associated fine-grained sedimentary rocks suggest temporally controlled variations in isotopic composition interpreted to represent two-component mixing between juvenile volcanic detritus and a more evolved detrital component. The succession of facies in the Harrison Lake Formation records initial basin subsidence in the Early Jurassic, initiation of explosive volcanism in the late early Toarcian, a change to effusive volcanism in the early Aalenian, and late-stage explosive volcanism in the late Bajocian. The Harrison Lake Formation contains mesoscopic folds and overturned bedding that are absent in the overlying Callovian Mysterious Creek Formation, strongly suggesting the existence of a regional Bathonian deformational event in the southern Coast Belt.
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Wright, Robert. "MODVOLC: 14 years of autonomous observations of effusive volcanism from space." Geological Society, London, Special Publications 426, no. 1 (August 27, 2015): 23–53. http://dx.doi.org/10.1144/sp426.12.

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Byrne, Paul K., Lillian R. Ostrach, Caleb I. Fassett, Clark R. Chapman, Brett W. Denevi, Alexander J. Evans, Christian Klimczak, Maria E. Banks, James W. Head, and Sean C. Solomon. "Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga." Geophysical Research Letters 43, no. 14 (July 21, 2016): 7408–16. http://dx.doi.org/10.1002/2016gl069412.

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Fink, Jonathan H., Steven W. Anderson, and Curtis R. Manley. "Textural constraints on effusive silicic volcanism: Beyond the permeable foam model." Journal of Geophysical Research 97, B6 (1992): 9073. http://dx.doi.org/10.1029/92jb00416.

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Busby, Cathy. "Possible distinguishing characteristics of very deepwater explosive and effusive silicic volcanism." Geology 33, no. 11 (2005): 845. http://dx.doi.org/10.1130/g21216.1.

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Dissertations / Theses on the topic "Volcanisme effusif"

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Samper, Agnès. "Etude géochronologique, aspects géomorphologiques et géochimiques du volcanisme de l’île de Basse Terre (Guadeloupe), et datation des structures d’effondrement de flanc majeures de l’arc des Petites Antilles." Paris 11, 2007. https://tel.archives-ouvertes.fr/tel-00398601.

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La technique K-Ar Cassignol-Gillot nous a permis de définir les limites temporelles du volcanisme effusif sub-aérien de l’île de Basse Terre, Guadeloupe, et de préciser les périodes d’activité des quatre massifs de l’île. Le Complexe Basal [2,79±0,04 - 2,68±0,04 Ma], la Chaîne Septentrionale [1,81±0,03 - 1,15±0,02 Ma], la Chaîne Axiale [1023±25 - 435±8 ka], le complexe de Grande-Découverte (GD) [205±28 - actuel] illustrent la migration du volcanisme à Basse Terre depuis 3 Ma suivant une direction principale N-S et une vitesse de 20 km/Ma. L’extraction des magmas serait contrôlée par les systèmes de graben E-W et failles normales en échelon NW-SE affectant la Guadeloupe. Les taux d’extrusion calculés sur la base d’observations et modélisations morphologiques vont de 1,4 10-5 à 4,5 10-4 km3/yr. Au sud du volcan de GD, les diverses phases d'activité effusive du complexe de Trois-Rivières-Madeleine montrent une contemporanéité avec celles du volcan de GD. Les coulées de Trois-Rivières (87±5 ka) puis l’alignement E-W Madeleine-Le Palmiste (70 à 45 ka) datent une phase de propagation du rift de Marie-Galante. Des coulées <15 ka dans l'environnement du dôme de la Madeleine permettent d’étendre à l’extrême sud de l’île la zone d’activité volcanique Holocène. L’aléa volcanique n’est plus restreint au Massif de Soufrière-GD mais doit être étendu en son sud au massif de Madeleine-Trois-Rivières. Des effondrements de flanc majeurs ont été datés sur les îles de Basse Terre (640 ka, 550 ka), Dominique (100 ka), Martinique (330 ka) et Sainte-Lucie (100 ka). Une relation causale entre la récurrence de ces phénomènes catastrophiques et les changements climatiques globaux est proposée
The K-Ar Cassignol-Gillot technique enabled us to define the temporal bounds of sub-aerial effusive volcanism in Basse Terre, Guadeloupe, and to constrain the periods of volcanic activity of the four massifs of the island. The Basal Complex [2. 79±0. 04 – 2. 68±0. 04 Ma], the Septentrional Chain [1. 81±0. 03 – 1. 15±0. 02 Ma], the Axial Chain [1023±25 - 435±8 ka] and the most recent volcanic complex of Grande-Découverte (GD) [205±28-present] illustrate the southwards migration of volcanism through time in Basse-Terre since 3 Ma, along a N-S main direction, at a rate of 20 km/Ma. We propose magma extraction to be linked to the E-W striking graben and N-S en-échelon normal fault systems affecting Guadeloupe. Extrusion rates, defined from morphological observations and modeling spread from 1. 4x10-5 to 4. 5x10-4 km3/yr. South of GD volcano, the several volcanic phases of the Trois Rivières–Madeleine Complex show to be contemporaneous with the GD volcano ones. The Trois-Rivières lava flows (87±5 ka) and subsequent emplacement of E-W alignment Madeleine-Le Palmiste (70 to 45 ka) constrain the age of a Marie-Galante rift propagation phase. Dating of lava flows <15 ka in the surroundings of the Madeleine dome lead to extend the Holocene volcanic zone up to the extreme south of the island, hence to consider volcanic hazards in a larger zone spreading from La Soufrière area up to the Madeleine -Trois Rivières volcanic complex. Finally, dating of major flank-collapse events in Basse Terre (640 and 550 ka), Dominica (100 ka), Martinique (330 ka) and St. Lucia (100 ka) have been realized; we propose a causal link between the recurrence of such catastrophic events and global climate changes
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Cáceres, Acevedo Francisco Andrés. "Magma storage conditions and eruptive dynamics of post-glacial effusive volcanism at Laguna del Maule Volcanic field." Tesis, Universidad de Chile, 2016. http://repositorio.uchile.cl/handle/2250/140208.

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Magíster en Ciencias, Mención Geología
Geólogo
La mayoría de los campos volcánicos monogenéticos están constituidos principalmente por productos piroclásticos de composición basáltica. Los volúmenes emitidos por cada centro eruptivo tienden a ser pequeños, menores a 1 km3, donde su actividad puede durar días a años, mientras que el campo volcánico completo se puede desarrollar y perdurar por millones de años, pudiendo superar en volumen a un volcán poligenético. En este sentido, el Campo Volcánico Laguna del Maule (CVLdM) representa un caso excepcional con más de 350 km3 de material basáltico a riolítico, eruptado mayormente de manera efusiva desde el Pleistoceno. En este trabajo se propone un modelo volcanológico-petrológico de la dinámica eruptiva de las lavas post-glaciales emplazadas en la parte Oeste del CVLdM, analizando la evolución del magma en profundidad, el ascenso de magma por los conductos eruptivos y el emplazamiento de lavas en superficie. Se estudió la morfometría, mineralogía y química de seis lavas y un domo del CVLdM para modelar las condiciones termodinámicas pre-eruptivas del magma y su evolución, incluyendo posibles procesos magmáticos causantes de su migración y ascenso a la superficie. Las lavas analizadas tienen una composición química andesítica a riolítica, morfología de bloques, volúmenes de 0.03 a 1.16 km3, largos máximos de 10 km, anchos máximos de 5 km y espesores máximos de 140 m. Los resultados indican la presencia de un sistema magmático formado en cuatro etapas, comenzando con la acumulación de magma andesítico basáltico a andesítico debido a múltiples intrusiones. Posteriormente, procesos de cristalización desarrollaron un reservorio tipo mush cristalino (13-17 km, 970-1025 °C) con extracción y ascenso de líquido intersticial. Una tercera etapa de estancamiento del magma en ascenso proveniente de la extracción más profunda (7-11 km, 900-970 °C), permitió la formación de un nuevo mush cristalino más evolucionado. Finalmente, una nueva extracción y ascenso del líquido intersticial riolítico formó un reservorio magmático riolítico pobre en cristales (~5 km, 760-800 °C) bajo el lago. El constante recalentamiento debido a múltiples intrusiones permitó al sistema magmático permanecer activo en el largo plazo, producto de variadas intrusiones de magma máfico en el caso del reservorio profundo y magma silícico en el caso del reservorio más somero.
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Book chapters on the topic "Volcanisme effusif"

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Fujibayashi, Norie, and Umio Sakai. "Vesiculation and eruption processes of submarine effusive and explosive rocks from the Middle Miocene Ogi Basalt, Sado Island, Japan." In Explosive Subaqueous Volcanism, 259–72. Washington, D. C.: American Geophysical Union, 2003. http://dx.doi.org/10.1029/140gm17.

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Murcia, Hugo, and Károly Németh. "Effusive Monogenetic Volcanism." In Volcanoes - Updates in Volcanology [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.94387.

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The study of monogenetic volcanism around Earth is rapidly growing due to the increasing recognition of monogenetic volcanic edifices in different tectonic settings. Far from the idea that this type of volcanism is both typically mafic and characteristic from intraplate environments, it occurs in a wide spectrum of composition and geological settings. This volcanism is widely known by the distinctive pyroclastic cones that represent both magmatic and phreatomagmatic explosive activity; they are known as scoria or spatter cones, tuff cones, tuff rings, maars and maar-diatremes. These cones are commonly associated with lava domes and usually accompanied by lava flows as part of their effusive eruptive phases. In spite of this, isolated effusive monogenetic emissions also appear around Earth’s surface. However, these isolated emissions are not habitually considered within the classification scheme of monogenetic volcanoes. Along with this, many of these effusive volcanoes also contrast with the belief that this volcanism is indicative of rapidly magma ascent from the asthenosphere, as many of the products are strongly evolved reflecting differentiation linked to stagnation during ascent. This has led to the understanding that the asthenosphere is not always the place that directly gives rise to the magma batches and rather, they detach from a crustal melt storage. This chapter introduces four singular effusive monogenetic volcanoes as part of the volcanic geoforms, highlights the fact that monogenetic volcanic fields can also be associated with crustal reservoirs, and outlines the processes that should occur to differentiate the magma before it is released as intermediate and acidic in composition. This chapter also provides an overview of this particular volcanism worldwide and contributes to the monogenetic comprehension for future studies.
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Stix, John. "Part III Effusive Volcanism." In The Encyclopedia of Volcanoes, 317–19. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-12-385938-9.02005-8.

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Ureta, Gabriel, Károly Németh, Felipe Aguilera, Matias Vilches, Mauricio Aguilera, Ivana Torres, José Pablo Sepúlveda, Alexander Scheinost, and Rodrigo González. "An Overview of the Mafic and Felsic Monogenetic Neogene to Quaternary Volcanism in the Central Andes, northern Chile (18-28°Lat.S)." In Volcanoes - Updates in Volcanology [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.93959.

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Monogenetic volcanism produces small eruptive volumes with short eruption history, different chemical compositions, and relatively simple conduit. The Central Volcanic Zone of the Andes is internationally known as a natural laboratory to study volcanism, where mafic and felsic products are present. In this contribution, the spectrum of architectures, range of eruptive styles, lithological features, and different magmatic processes of the mafic and felsic monogenetic Neogene to Quaternary volcanoes from the Central Volcanic Zone of the Andes in northern Chile (18°S-28°S) are described. The major volcanic activity occurred during the Pleistocene, where the most abundant activity corresponds to effusive and Strombolian eruptions. This volcanism is characterized by external (e.g., magma reservoirs or groundwater availability) and internal (e.g., magma ascent rate or interaction en-route to the surface) conditions, which determine the changes in eruptive style, lithofacies, and magmatic processes involved in the formation of monogenetic volcanoes.
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Conference papers on the topic "Volcanisme effusif"

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Ludlam, Abadie. "DECOMPRESSION AND HEATING INDUCED AMPHIBOLE BREAKDOWN IN EFFUSIVE VOLCANISM ON DOMINICA, LESSER ANTILLES." In Keck Proceedings. Keck Geology Consortium, 2018. http://dx.doi.org/10.18277/akrsg.2019.31.14.

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McBride, Marie J., Briony Horgan, and Samuel J. Lawrence. "SPECTRAL ANALYSIS OF EXPLOSIVE AND EFFUSIVE VOLCANISM IN THE MARIUS HILLS VOLCANIC COMPLEX." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321659.

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Bersson, Jessica. "EXPLOSIVE TO EFFUSIVE TRANSITION IN INTERMEDIATE VOLCANISM: AN ANALYSIS OF CHANGING MAGMA SYSTEM CONDITIONS IN DOMINICA." In Keck Proceedings. Keck Geology Consortium, 2018. http://dx.doi.org/10.18277/akrsg.2019.31.05.

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Brueseke, Matthew E., and David A. Martin. "GLASS AND CRYSTAL CHEMISTRY FROM MIOCENE JARBIDGE RHYOLITE LAVAS (NEVADA, USA): CONSTRAINTS ON CRYSTAL-RICH RHYOLITE PETROGENESIS AND EFFUSIVE VOLCANISM." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-326539.

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Ward, Peter L. "HOW VARIATIONS IN THE RATES OF EFFUSIVE BASALTIC FLOOD VOLCANISM VERSUS AEROSOL-FORMING EXPLOSIVE VOLCANISM HAVE DRIVEN CLIMATE CHANGE AND RATES OF MASS EXTINCTION THROUGHOUT EARTH HISTORY AND HOW HUMANS HAVE MODIFIED THIS INTERACTION." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283876.

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