Relevant bibliographies by topics / Volcanism

Contents

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

Academic literature on the topic 'Volcanism'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 July 2025

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Journal articles on the topic "Volcanism"

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Tripathi, C. "Volcanism in Gondwanas." Journal of Palaeosciences 36 (December 31, 1987): 285–89. http://dx.doi.org/10.54991/jop.1987.1587.

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In India the Lower Permian event is marked by a major volcanic episode in the Himalayan belt and rift faulting in the Peninsula which gave rise to various Gondwana basins. The Lower Cretaceous major volcanic episode represented by the Rajmahal Trap represents the termination of Gondwana sedimentation. Lower Permian volcanism is represented by the Panjal Volcanics in Kashmir Basin and its equivalent, the Volcanics in Spiti-Zanskar Basin and Rotung Volcanics (Abor Volcanics) in Arunachal Pradesh. In Karakarom Basin of Ladakh, volcanism is associated with Changtash and Aqtash formations of Permia
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McDOUGALL, IAN. "Age of volcanism and its migration in the Samoa Islands." Geological Magazine 147, no. 5 (2010): 705–17. http://dx.doi.org/10.1017/s0016756810000038.

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AbstractPotassium–argon (K–Ar) ages on whole rock samples have been measured on lavas from the subaerial Samoa Islands, which form a broadly linear volcanic chain that extends from the ESE to the WNW for about 360 km. The Manu'a Islands near the southeast limit of the chain exhibit youthful ages, with most <0.4 Ma, in keeping with the geological observations. Tutuila consists of several volcanoes, and previous work yielded a mean K–Ar age of 1.26 ± 0.15 Ma for the shield-building volcanism. Upolu, to the WNW of Tutuila, gives a mean age of 2.15 ± 0.35 Ma for the shield-building phase, repre
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Smellie, John L. "Chapter 3.2a Bransfield Strait and James Ross Island: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 227–84. http://dx.doi.org/10.1144/m55-2018-58.

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AbstractFollowing more than 25 years of exploration and research since the last regional appraisal, the number of known subaerially exposed volcanoes in the northern Antarctic Peninsula region has more than trebled, from less than 15 to more than 50, and that total must be increased at least three-fold if seamounts in Bransfield Strait are included. Several volcanoes remain unvisited and there are relatively few detailed studies. The region includes Deception Island, the most prolific active volcano in Antarctica, and Mount Haddington, the largest volcano in Antarctica. The tectonic environmen
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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 sti
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Ganelin, A. V., E. V. Vatrushkina, and M. V. Luchitskaya. "Geochemistry and geochronology of cretaceous volcanism of Chauna region, Central Chukotka." Геохимия 64, no. 1 (2019): 20–42. http://dx.doi.org/10.31857/s0016-752564120-42.

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New geochronological and geochemical data on the age and composition of Cretaceous volcanism of Palyavaam River basin (Central Chukotka, Chauna region) are presented. First complex is composed of rhyolites, ignimbrites and felsic tuffs of Chauna Group of Okhotsk-Chukotka volcanic belt (OCVB). Second complex is represented by volcanic rocks of latite-shoshonite series of Early Cretaceous age, distinguished as Etchikun’ Formation. Its origin is still debatable. Some researchers refer deposits of Etchikun’ Formation to magmatic stage before OCVB activity. Other authors include in Chauna Group com
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SIMKIN, T. "Monitoring Volcanism: Volcanic Hazards." Science 245, no. 4913 (1989): 83–84. http://dx.doi.org/10.1126/science.245.4913.83.

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Kitsopoulos, K. "MAGMA GENERATION AND MIXING IN THE EARLIEST VOLCANIC CENTRE OF SANTORINI (AKROTIRI PENINSULA). MINERAL CHEMISTRY EVIDENCE FROM THE AKROTIRI PYROCLASTICS." Bulletin of the Geological Society of Greece 43, no. 5 (2017): 2625. http://dx.doi.org/10.12681/bgsg.11669.

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Santorini is a dominant expression of magma generation and subsequent volcanism in the Meditereanean area, where a calk-alkaline, high-alumina, basalt-andesite-dacite type of volcanism was expressed from eight centres. The volcanics of the Akrotiri peninsula are considered to be the products of the earliest (Pliocene Pleistocene) volcanic centre. The present study has investigated the mineral chemistry of some major pyrogenic phenocrysts, such as plagioclase and Fe-Ti oxides, of the Akrotiri pyroclatics unit, which have undergone a notable zeolitization procedure. The results are compatible wi
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Ludden, John, Claude Hubert, and Clement Gariépy. "The tectonic evolution of the Abitibi greenstone belt of Canada." Geological Magazine 123, no. 2 (1986): 153–66. http://dx.doi.org/10.1017/s0016756800029800.

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AbstractBased on structural, geochemical, sedimentological and geochronological studies, we have formulated a model for the evolution of the late Archaean Abitibi greenstone belt of the Superior Province of Canada. The southern volcanic zone (SVZ) of the belt is dominated by komatiitic to tholeiitic volcanic plateaux and large, bimodal, mafic-felsic volcanic centres. These volcanic rocks were erupted between approximately 2710 Ma and 2700 Ma in a series of rift basins formed as a result of wrench-fault tectonics.The SVZ superimposes an older volcanic terrane which is characterized in the north
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CITRONI, SERGIO B., MIGUEL A. S. BASEI, OSWALDO SIGA JR., and JOSÉ M. DOS REIS NETO. "Volcanism and stratigraphy of the Neoproterozoic Campo Alegre Basin, SC, Brazil." Anais da Academia Brasileira de Ciências 73, no. 4 (2001): 581–97. http://dx.doi.org/10.1590/s0001-37652001000400012.

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The depositional succession of the Campo Alegre Basin (Santa Catarina - southern Brazil) was investigated having the evolution of the volcanic activity as background. The different stratigraphic units are interpreted as belonging to different volcanic stages: Bateias Formation, conglomerates and sandstones, related with a pre-volcanic stage; Campo Alegre Group, at the main volcanic stage, with each different formation corresponding to different episodes of volcanism - Rio Negrinho Formation, corresponding to the basic volcanism, Avenca Grande Formation to ignimbritic event, Serra de São Miguel
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Griffiths, Chris J., and Richard D. J. Oglethorpe. "The stratigraphy and geochronology of Adelaide Island." Antarctic Science 10, no. 4 (1998): 462–75. http://dx.doi.org/10.1017/s095410209800056x.

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The Mesozoic-Cenozoic volcanic arc of the Antarctic Peninsula is represented on Adelaide Island by a sedimentary and volcanic succession intruded by plutons. 40Ar-39 Ar step-heating age spectra have been obtained from volcanic rocks and hornblende separates from sedimentary clasts of plutonic origin. These spectra show evidence for some argon loss, but, in general, have plateau ages which are consistent with the mapped stratigraphy and with other geochronological controls, suggesting that they approximate to original ages. As a result the following events in the evolution of Adelaide Island ca
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Dissertations / Theses on the topic "Volcanism"

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Smith, R. T. "Eruptive and depositional models for units 3 and 4 of the 1.85 ka Taupo eruption: Implications for the nature of large-scale 'wet' eruptions." Thesis, University of Canterbury. Geological Science, 1998. http://hdl.handle.net/10092/5928.

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Phreatomagmatic eruptions result from the explosive interaction between magma and some external source of water, and produce deposits which are usually distinctive in nature from those of magmatic eruptions. The widespread deposits of large-scale phreatomagmatic eruptions (usually termed Phreatoplinian) are poorly studied relative to their magmatic counterparts and, consequently, current models for large-scale phreatomagmatic volcanism remain speculative. The Hatepe ash and Rotongaio ash (units 3 and 4 of the 1.85 ka Taupo eruption) are two classical widespread phreatomagmatic fall deposits. T
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Hellwig, Bridget M. "The viscosity of dacitic liquids measured at conditions relevant to explosive arc volcanism determing the influence of temperature, silicate composition, and dissolved volatile content /." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4597.

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Thesis (M.S.)--University of Missouri-Columbia, 2006.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (February 7, 2007) Includes bibliographical references.
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Watson, Sarah Penelope. "Hotspots and volcanism." Thesis, University of Cambridge, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.386840.

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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.

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The explosive events in Teide Pico Viejo (TPV) complex in Tenerife Island (Spain) have traditionally been restricted to the subplinian eruption of Montaña Blanca, which occurred about 2000 years ago. A recent revision of the stratigraphy of TPV shows that phonolitic explosive activity has been significant during the Holocene, with several distinct episodes related to eruptions ranging from Strombolian to sub-plinian. Using field, mineralogical and geochemical stratigraphic correlations, we have identified 11 phonolitic explosive eruptions related to the satellite domes present all around TPV
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Watt, Sebastian F. L. "Records of volcanism and controls on volcanic processes in southern Chile." Thesis, University of Oxford, 2010. http://ora.ox.ac.uk/objects/uuid:41cf206e-2cef-4108-9267-5e9217aee96d.

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This thesis describes volcanic records from the Andean southern volcanic zone, based on the collection of field data between Calbuco and Puyuhuapi volcanic centres, with a particular focus on the Hualaihue peninsula, combined with existing records from the region as a whole. These data, extending the understanding of the volcanic history of southern Chile, are examined for evidence of spatial or temporal variability, which may be used to explore underlying controls on volcanic processes. All three volcanoes on the Hualaihue peninsula have been active in the Holocene. A large mafic scoria unit
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Buck, Adrian. "The Mt. Marcella volcanics : middle Triassic convergent margin volcanism in Southeast Queensland." Thesis, Queensland University of Technology, 2008. https://eprints.qut.edu.au/20171/1/Adrian_Buck_Thesis.pdf.

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Triassic igneous rocks in southeast Queensland show a number of subduction related geochemical characteristics. Extensive calc-alkalic granitoids chains characterise the region and define the ancient arc setting. Despite good evidence that an arc was present, Triassic volcanic rocks are relatively sparse in southeast Queensland. The Mt Marcella Volcanics, of the northern Esk Trough are a previously poorly understood piece of the Middle Triassic convergent margin of southeast Queensland. A three stage model is proposed for the eruptive development of the Middle Triassic (245- 230Ma) volcanic su
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Buck, Adrian. "The Mt. Marcella volcanics : middle Triassic convergent margin volcanism in Southeast Queensland." Queensland University of Technology, 2008. http://eprints.qut.edu.au/20171/.

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Triassic igneous rocks in southeast Queensland show a number of subduction related geochemical characteristics. Extensive calc-alkalic granitoids chains characterise the region and define the ancient arc setting. Despite good evidence that an arc was present, Triassic volcanic rocks are relatively sparse in southeast Queensland. The Mt Marcella Volcanics, of the northern Esk Trough are a previously poorly understood piece of the Middle Triassic convergent margin of southeast Queensland. A three stage model is proposed for the eruptive development of the Middle Triassic (245- 230Ma) volcanic su
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Hartley, Margaret Elizabeth. "Post glacial volcanism and magmatism on the Askja volcanic system, North Iceland." Thesis, University of Edinburgh, 2012. http://hdl.handle.net/1842/5845.

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Postglacial activity on the Askja volcanic system, north Iceland, has been dominated by basaltic volcanism. Over 80% of Askja's postglacial basalts fall within a relatively narrow compositional range containing between 4 and 8 wt.% MgO. The 'main series' is further divided into two groups separated by a distinct compositional gap evident in major and trace element concentrations. The most evolved basalts formed by fractional crystallisation within shallow magma reservoirs, followed by the extraction of residual liquid from a semi-rigid, interconnected crystal network. This process is analogous
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Spinks, Karl D. "Rift architecture and Caldera volcanism in the Taupo Volcanic Zone, New Zealand." Thesis, University of Canterbury. Geological Sciences, 2005. http://hdl.handle.net/10092/4944.

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The Taupo Volcanic Zone (TVZ) is investigated to determine the interaction of regional structure and volcanism. A three-tiered approach is employed involving (i) analysis of rift geometry and segmentation in Modem TVZ(<300 ka) from remote sensing and digital topographic data; (ii) fault kinematic data collected along the length of TVZ; and (iii) combining new and existing volcanological data for TVZ. Modem TVZ is a NNE-SSW trending intra-arc rift zone, subject to dextral transtension, and characterised by a segmented axial rift zone with a number of offset and variably oriented rift segments.
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Carn, Simon Anthony. "Persistent volcanism in Indonesia." Thesis, University of Cambridge, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.624364.

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Books on the topic "Volcanism"

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Ollier, Cliff. Volcanoes. Basil Blackwell, 1988.

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H, Stauffer Peter, Decker Robert Wayne 1927-, and Wright Thomas L. 1935-, eds. Volcanism in Hawaii. U.S. Geological Survey, 1987.

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Ollier, Cliff. Volcanoes. Blackwell, 1988.

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Schmincke, Hans-Ulrich. Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4.

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Bardintzeff, Jacques-Marie. Les volcans. Editions Minerva, 2004.

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Bardintzeff, Jacques-Marie. Les volcans. Liber, 1997.

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Bell, Keith, and Jörg Keller, eds. Carbonatite Volcanism. Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-79182-6.

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Robert, Lattanzio, Sadd James, Stansfield David, Corporation for Community College Television., and Magic Lantern Communications, eds. Volcanism [videorecording]. CCC Television, 1992.

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Faraone, Domenico. I vulcani e l'uomo: Miti, leggende e storia. Liguori, 2002.

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Jean-Claude, Thouret, Chester David K, Ollier Cliff, Joyce B, and International Association of Geomorphology. Working Group on "Volcanic Geomorphology"., eds. Volcanic landforms, processes and hazards. Gebrüder Borntraeger, 2005.

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Book chapters on the topic "Volcanism"

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Schmincke, Hans-Ulrich. "Introduction." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_1.

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Schmincke, Hans-Ulrich. "Strombolian, Hawaiian and Plinian Eruptions and the Mount St. Helens Eruption 1980." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_10.

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Schmincke, Hans-Ulrich. "Pyroclastic Flows, Block and Ash Flows, Surges and the Laacher See Eruption." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_11.

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Schmincke, Hans-Ulrich. "Fire and Water." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_12.

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Schmincke, Hans-Ulrich. "Volcanic Hazards, Volcanic Catastrophes, and Disaster Mitigation." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_13.

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Schmincke, Hans-Ulrich. "Volcanoes and Climate." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_14.

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Schmincke, Hans-Ulrich. "Man and Volcanoes: The Benefits." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_15.

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Schmincke, Hans-Ulrich. "Plate Tectonics." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_2.

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Schmincke, Hans-Ulrich. "Magma." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_3.

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Schmincke, Hans-Ulrich. "Rheology, Magmatic Gases, Bubbles and Triggering of Eruptions." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_4.

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Conference papers on the topic "Volcanism"

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Зонов, Ю. Б., and О. В. Левченко. "ZONING OF LANDSCAPES AREAS OF THE MODERN VOLCANISM OF KAMCHATKA." In Геосистемы Северо-Восточной Азии. Crossref, 2021. http://dx.doi.org/10.35735/tig.2021.11.81.016.

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В настоящей статье сделана попытка провести зонирование ландшафтов районов современного вулканизма Камчатки и выявить пространства с типовыми природными признаками. Эти признаки напрямую коррелируются со степенью интенсивности и характером проявления современного вулканизма. Рассматривается ландшафтообразующая роль современного вулканизма, которая заключается в модификации ландшафтов различного ранга в зависимости от объёма и типа поступающего вулканического материала. In this article, an attempt is made to zoning the landscapes of the areas of modern volcanism in Kamchatka and to identify spa
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Satyana, A. H. "Trilogy Of Southeast Sundaland Terranes: Re-Uniting Drifted Terranes of Southeast Sundaland Using Common Marker ff The Late Cretaceous Volcanics to Volcanic-Clastics of The Meratus Mountains, South Sulawesi, And Sumba - Implications For Petroleum Opportunities." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-39.

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Amalgamation and dispersion of terranes characterized the growth and slivering of Southeast Sundaland into the present configuration of central Indonesia. Amalgamation of the Paternoster-West Sulawesi terrane which docked, in mid-Cretaceous time, onto the Southwest Borneo terrane, thus closed the Meso-Tethys Ocean at the Meratus suture. This made Sundaland expand its area to the east and southeast. In the Late Cretaceous time, the Ceno-Tethys oceanic plate subducted beneath Southeast Sundaland, giving rise to coeval volcanism in the Meratus Mountains and the surrounding areas. Dispersion of so
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Blatter, Dawnika, Seth Burgess, and Julie M. Donnelly-Nolan. "EARLY PRIMITIVE VOLCANISM AT CLEAR LAKE VOLCANIC FIELD, CA." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363121.

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Bonessi, Jacob M., Tyrone O. Rooney, Andrew LaVigne, et al. "SILICIC VOLCANISM OF THE PORCUPINE VOLCANICS: IMPLICATIONS FOR MAGMA DIFFERENTIATION DURING THE TERMINAL STAGES OF VOLCANISM WITHIN THE MIDCONTINENT RIFT." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321887.

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Grunder, Anita, and Martin J. Streck. "SILICIC VOLCANISM AS A TRACER FOR COLUMBIA RIVER FLOOD BASALT VOLCANISM." In Joint 120th Annual Cordilleran/74th Annual Rocky Mountain Section Meeting - 2024. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024cd-399658.

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Guliyev, Ibrahim S. "Mud Volcanism in Azerbaijan." In RECENT GEODYNAMICS, GEORISK AND SUSTAINABLE DEVELOPMENT IN THE BLACK SEA TO CASPIAN SEA REGION. AIP, 2006. http://dx.doi.org/10.1063/1.2190728.

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Hou, Dongmei, Chao Li, Pengyu Gao, Xun Yuan, Xiaolong Zhang, and Zhong Cheng. "Sedimentary Evolution of Delta and Reservoir Distribution Under the Control of a Volcanic System." In ADIPEC. SPE, 2023. http://dx.doi.org/10.2118/215985-ms.

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Abstract The BZ34-9 oilfield is a clastic reservoir discovered in the Oligocene strata in the southern part of the Bohai Bay Basin. The volcanic system here is intermixed with a clastic reservoir that spans more than 1000 meters. In its upper part, it overlies about 2000 meters of Miocene strata. Volcanic activity has influenced the deposition and filling of the lacustrine and played a key role in controlling the distribution of clastic reservoirs. Based on 3D seismic data and lithological data from 74 wells, four types of volcanic were identified and extracted according to seismic sequences.
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Ackerson, Michael R., Todd K. Knobbe, Elizabeth Pettitt, E. Bruce Watson, and Morgan F. Schaller. "WHERE VOLCANISM AND THE ATMOSPHERE MEET: GAS COMPOSITIONS OF VOLCANIC PUMICE CLASTS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323344.

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Streck, Martin J., William McIntosh, and Mark L. Ferns. "CO-CRBG RHYOLITE VOLCANISM REASSESSED." In 68th Annual Rocky Mountain GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016rm-276108.

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King, Scott D. "STABLE HOTSPOT VOLCANISM ON VENUS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318245.

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Reports on the topic "Volcanism"

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Heiken, G., D. Krier, and M. G. Snow. Intracaldera volcanism and sedimentation - Creede Caldera, Colorado. Office of Scientific and Technical Information (OSTI), 1997. http://dx.doi.org/10.2172/484542.

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Edwards, B. R., J. K. Russell, R. G. Anderson, and M. Harder. Overview of Neogene to Recent volcanism in the Atlin volcanic district, Northern Cordilleran volcanic province, northwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214025.

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Jackson, L. E. Pleistocene Subglacial Volcanism near Fort Selkirk, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127498.

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Bruce M. Crowe, Frank V. Perry, Greg A. Valentine, and Lynn M. Bowker. Volcanism Studies: Final Report for the Yucca Mountain Project. Office of Scientific and Technical Information (OSTI), 1998. http://dx.doi.org/10.2172/12111.

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Fallas, K. M., and W. Matthews. Age dating of a bentonite in the Duo Lake Formation, western Mackenzie Mountains, Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328830.

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In the Misty Creek Embayment of the western Mackenzie Mountains, Duo Lake Formation locally includes minor volcanic deposits associated with Marmot Formation volcanism. A bentonite layer from an outcrop of graptolitic shale found in NTS map area 106-B, in the upper part of the Duo Lake Formation, was sampled for U-Pb zircon dating. Analytical results yielded a dominant population of grains with a concordia age of 439.8 ± 3.0 Ma, interpreted as the age of deposition. Minor inherited zircon populations yielded ages ranging from approximately 1200 to 2850 Ma. Observed graptolites from the same ou
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6

Hickson, C. J. Character of volcanism, volcanic hazards, and risk, northern end of the Cascade magmatic arc, British Columbia and Washington State. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/203253.

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Klöcking, M., K. Czarnota, D. C. Champion, A. L. Jaques, and D. R. Davies. Spatio-temporal evolution of Australian lithosphere-asthenosphere boundary from mafic volcanism. Geoscience Australia, 2020. http://dx.doi.org/10.11636/135075.

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Valentine, G. A., and J. E. Bossert. Numerical simulation of explosive volcanism and its effects on the atmosphere. Office of Scientific and Technical Information (OSTI), 1998. http://dx.doi.org/10.2172/334239.

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Mortensen, J. K., R. I. Thorpe, W. A. Padgham, J. E. King, and W J Davis. U-Pb zircon ages for felsic volcanism in Slave Porvince, N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/126606.

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Crowe, B., F. Perry, M. Murrell, et al. Status of volcanism studies for the Yucca Mountain Site Characterization Project. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/42463.

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