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Journal articles on the topic 'Volcanisme intraplaque'

Author: Grafiati

Published: 4 June 2021

Last updated: 5 February 2022

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1

Ouali, Houssa, Bernard Briand, Jean-Luc Bouchardon, and Mohamed El Maâtaoui. "Mise en évidence d'un volcanisme alcalin intraplaque d'âge Acadien dans la Meseta nord-occidentale (Maroc)." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 330, no. 9 (2000): 611–16. http://dx.doi.org/10.1016/s1251-8050(00)00166-x.

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2

Aït Chayeb, E. H., N. Youbi, A. El-Boukhari, M. Bouabdelli, and M. Amrhar. "Le volcanisme permien et mésozoïque inférieur du bassin d'Argana (Haut-Atlas occidental, Maroc): un magmatisme intraplaque associé à l'ouverture de l'Atlantique central." Journal of African Earth Sciences 26, no. 4 (1998): 499–519. http://dx.doi.org/10.1016/s0899-5362(98)00029-3.

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3

GUEZAL, J., M. BAGHDADI, and A. BARAKAT. "Les Basaltes de l’Atlas de Béni-Mellal (Haut Atlas Central, Maroc): un Volcanisme Transitionnel Intraplaque Associé aux Stades de L’évolution Géodynamique du Domaine Atlasique." Anuário do Instituto de Geociências - UFRJ 36_2, no. 1 (2013): 70–85. http://dx.doi.org/10.11137/2013_2_70_85.

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4

Lee, Cin-Ty A., and Stephen P. Grand. "Intraplate volcanism." Nature 482, no. 7385 (2012): 314–15. http://dx.doi.org/10.1038/482314a.

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5

Butterworth, N. P., R. D. Müller, L. Quevedo, J. M. O'Connor, K. Hoernle, and G. Morra. "Pacific plate slab pull and intraplate deformation in the early Cenozoic." Solid Earth 5, no. 2 (2014): 757–77. http://dx.doi.org/10.5194/se-5-757-2014.

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Abstract. Large tectonic plates are known to be susceptible to internal deformation, leading to a~range of phenomena including intraplate volcanism. However, the space and time dependence of intraplate deformation and its relationship with changing plate boundary configurations, subducting slab geometries, and absolute plate motion is poorly understood. We utilise a buoyancy-driven Stokes flow solver, BEM-Earth, to investigate the contribution of subducting slabs through time on Pacific plate motion and plate-scale deformation, and how this is linked to intraplate volcanism. We produce a serie

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6

Butterworth, N. P., R. D. Müller, L. Quevedo, J. M.O'Connor, K. Hoernle, and G. Morra. "Pacific Plate slab pull and intraplate deformation in the early Cenozoic." Solid Earth Discussions 6, no. 1 (2014): 145–90. http://dx.doi.org/10.5194/sed-6-145-2014.

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Abstract. Large tectonic plates are known to be susceptible to internal deformation, leading to a range of phenomena including intraplate volcanism. However, the space and time dependence of intraplate deformation and its relationship with changing plate boundary configurations, subducting slab geometries, and absolute plate motion is poorly understood. We utilise a buoyancy driven Stokes flow solver, BEM-Earth, to investigate the contribution of subducting slabs through time on Pacific Plate motion and plate-scale deformation, and how this is linked to intraplate volcanism. We produce a serie

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7

Mather, Ben R., R. Dietmar Müller, Maria Seton, Saskia Ruttor, Oliver Nebel, and Nick Mortimer. "Intraplate volcanism triggered by bursts in slab flux." Science Advances 6, no. 51 (2020): eabd0953. http://dx.doi.org/10.1126/sciadv.abd0953.

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Long-lived, widespread intraplate volcanism without age progression is one of the most controversial features of plate tectonics. Previously proposed edge-driven convection, asthenospheric shear, and lithospheric detachment fail to explain the ~5000-km-wide intraplate volcanic province from eastern Australia to Zealandia. We model the subducted slab volume over 100 million years and find that slab flux drives volcanic eruption frequency, indicating stimulation of an enriched mantle transition zone reservoir. Volcanic isotope geochemistry allows us to distinguish a high-μ (HIMU) reservoir [>

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8

Leeman, William P. "Intraplate volcanism in eastern Australia and New Zealand." Geochimica et Cosmochimica Acta 61, no. 10 (1997): 2147–48. http://dx.doi.org/10.1016/s0016-7037(97)83224-3.

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9

Conrad, Clinton P., Todd A. Bianco, Eugene I. Smith, and Paul Wessel. "Patterns of intraplate volcanism controlled by asthenospheric shear." Nature Geoscience 4, no. 5 (2011): 317–21. http://dx.doi.org/10.1038/ngeo1111.

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10

Wadsworth, W. J. "Intraplate volcanism in Eastern Australia and New Zealand." Journal of Structural Geology 14, no. 3 (1992): 379–80. http://dx.doi.org/10.1016/0191-8141(92)90097-g.

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11

FITTON, GODFREY. "Intraplate Volcanism in Eastern Australia and New Zealand." Geophysical Journal International 105, no. 3 (1991): 805. http://dx.doi.org/10.1111/j.1365-246x.1991.tb00815.x.

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12

Thompson, R. N. "Intraplate volcanism in eastern Australia and New Zealand." Physics of the Earth and Planetary Interiors 65, no. 3-5 (1991): 337–38. http://dx.doi.org/10.1016/0031-9201(91)90139-9.

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13

Geldmacher, Jörg, Kaj Hoernle, Barry B. Hanan, et al. "Hafnium isotopic variations in East Atlantic intraplate volcanism." Contributions to Mineralogy and Petrology 162, no. 1 (2010): 21–36. http://dx.doi.org/10.1007/s00410-010-0580-5.

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14

van den Hove, Jackson C., Jozua Van Otterloo, Peter G. Betts, Laurent Ailleres, and Ray A. F. Cas. "Controls on volcanism at intraplate basaltic volcanic fields." Earth and Planetary Science Letters 459 (February 2017): 36–47. http://dx.doi.org/10.1016/j.epsl.2016.11.008.

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15

Cole, J. W. "Intraplate volcanism in Eastern Australia and New Zealand." Journal of Volcanology and Geothermal Research 46, no. 3-4 (1991): 331–32. http://dx.doi.org/10.1016/0377-0273(91)90092-e.

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16

Cebull, S. E., and D. H. Shurbet. "MEXICAN VOLVANIC BELT: AN INTRAPLATE TRANSFORM?" Geofísica Internacional 26, no. 1 (1987): 1–13. http://dx.doi.org/10.22201/igeof.00167169p.1987.26.1.1187.

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La evidencia temporal y "geométrica" sugiere que varios eventos regionales tectónicos fueron contribuyentes de mucha importancia durante la evolución del Cinturón Volcánico Mexicano (CVM). Estos incluyen (1) el desarrollo de una zona tectónica de debilidad en el área del actual CVM, seguido durante la época cenozoica por (2) actividad tectónica en la región caribe, que incluye la difusión a lo largo del fondo del mar en la depresión Caimán (3) cesación progresiva de subducción hacia el Sur, a lo largo de la costa poniente de Norteamérica y Centroamérica, y (4) desarrollo del proto-Golfo, el Go

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17

Yang, Jianfeng, and Manuele Faccenda. "Intraplate volcanism originating from upwelling hydrous mantle transition zone." Nature 579, no. 7797 (2020): 88–91. http://dx.doi.org/10.1038/s41586-020-2045-y.

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18

Davies, D. Rhodri, and Nicholas Rawlinson. "On the origin of recent intraplate volcanism in Australia." Geology 42, no. 12 (2014): 1031–34. http://dx.doi.org/10.1130/g36093.1.

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19

Raddick, M. Jordan, E. M. Parmentier, and Daniel S. Scheirer. "Buoyant decompression melting: A possible mechanism for intraplate volcanism." Journal of Geophysical Research: Solid Earth 107, B10 (2002): ECV 7–1—ECV 7–14. http://dx.doi.org/10.1029/2001jb000617.

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20

Uenzelmann-Neben, Gabriele, Daniela N. Schmidt, Frank Niessen, and Rüdiger Stein. "Intraplate volcanism off South Greenland: caused by glacial rebound?" Geophysical Journal International 190, no. 1 (2012): 1–7. http://dx.doi.org/10.1111/j.1365-246x.2012.05468.x.

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21

Yang, Fan, M. Santosh, Sung Won Kim, Hongying Zhou, and Youn Joong Jeong. "Late Mesozoic intraplate rhyolitic volcanism in the North China Craton: Far-field effect of the westward subduction of the Paleo-Pacific Plate." GSA Bulletin 132, no. 1-2 (2019): 291–309. http://dx.doi.org/10.1130/b35123.1.

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Abstract The Late Mesozoic was characterized by extensive volcanism, crustal extension, lithospheric thinning, and craton destruction in the North China Craton (NCC). Here we investigate the petrology, whole-rock geochemistry, zircon U-Pb geochronology, and Lu-Hf isotope of rhyolitic rocks from the Chicheng region of China along the northern margin of the NCC to constrain their petrogenesis, magma evolution, and associated geodynamic processes. The newly obtained zircon U-Pb age data constrain the eruption age of rhyolitic rocks at ca. 144–114 Ma during the Early Cretaceous with multiple magma

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22

Mukhopadhyay, Ranadhir. "Post-Cretaceous intraplate volcanism in the Central Indian Ocean Basin." Marine Geology 151, no. 1-4 (1998): 135–42. http://dx.doi.org/10.1016/s0025-3227(98)00073-5.

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23

Smith, A. D. "Recycling of oceanic crust and the origin of intraplate volcanism." Australian Journal of Earth Sciences 60, no. 6-7 (2013): 675–80. http://dx.doi.org/10.1080/08120099.2013.838188.

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24

Beier, Christoph, Wolfgang Bach, Alexander V. Busch, Felix S. Genske, Christian Hübscher, and Stefan H. Krumm. "Extreme intensity of fluid-rock interaction during extensive intraplate volcanism." Geochimica et Cosmochimica Acta 257 (July 2019): 26–48. http://dx.doi.org/10.1016/j.gca.2019.04.017.

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25

Hardman, Jonathon P. A., Simon P. Holford, Nick Schofield, Mark Bunch, and Daniel Gibbins. "The Warnie volcanic province: Jurassic intraplate volcanism in Central Australia." Gondwana Research 76 (December 2019): 322–47. http://dx.doi.org/10.1016/j.gr.2019.06.012.

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26

Dawson, J. B. "Neogene–Recent rifting and volcanism in northern Tanzania: relevance for comparisons between the Gardar province and the East African Rift valley." Mineralogical Magazine 61, no. 407 (1997): 543–48. http://dx.doi.org/10.1180/minmag.1997.061.407.06.

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AbstractThe tectonic position of the intraplate, alkaline volcanic province of N. Tanzania in a broad rift-controlled area astride the boundary between the Tanzania Craton and the circum-cratonic Mozambique Fold Belt, strongly resembles that of the Gardar province of S. Greenland. Earlier-identified petrological analogies between Gardar magmatism and that in the Kenya sector of the East African Rift Valley can be extended to volcanism in N. Tanzania, and analogies specifically with the Gardar agpaitic suite are strengthened by the occurrence of eudialyte and aenigmatite in some Tanzanian peral

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27

Sokolov, S. Yu. "The depth geodynamic state and its correlation with the surface geological and geophysical parameters along the sublatitudinal profile of Eurasia." Geodynamics & Tectonophysics 10, no. 4 (2019): 945–57. http://dx.doi.org/10.5800/gt-2019-10-4-0451.

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A cross‐sections of longitudinal (P) and transverse (S) wave anomalies (attribute δ(VP/VS)) is constructed along the sublatitudinal profile from the Atlantic Ocean to the Pacific Ocean across the regions of the latest Eurasian volcanism. It is correlated with surface geophysical parameters interpretable in terms of geodynamics: heat flow, seismicity and integrated conductivity of the lithosphere. All the volcanic groups are related to the negative anomalies of S‐ and P‐wave velocity variations at depths, which are observed in the eastern part of the profile from Central Asia to the Pacific Oce

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28

Aivazpourporgou, Sahereh, Stephan Thiel, Patrick C. Hayman, Louis N. Moresi, and Graham Heinson. "Decompression melting driving intraplate volcanism in Australia: Evidence from magnetotelluric sounding." Geophysical Research Letters 42, no. 2 (2015): 346–54. http://dx.doi.org/10.1002/2014gl060088.

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29

Fu, Yuanyuan V., Yuan Gao, Aibing Li, Lun Li, Yutao Shi, and Yi Zhang. "Origin of intraplate volcanism in northeast China from Love wave constraints." Journal of Geophysical Research: Solid Earth 121, no. 11 (2016): 8099–112. http://dx.doi.org/10.1002/2016jb013305.

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30

Hoernle, K., J. D. L. White, P. van den Bogaard, et al. "Cenozoic intraplate volcanism on New Zealand: Upwelling induced by lithospheric removal." Earth and Planetary Science Letters 248, no. 1-2 (2006): 350–67. http://dx.doi.org/10.1016/j.epsl.2006.06.001.

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31

Timm, Christian, Kaj Hoernle, Reinhard Werner, et al. "Temporal and geochemical evolution of the Cenozoic intraplate volcanism of Zealandia." Earth-Science Reviews 98, no. 1-2 (2010): 38–64. http://dx.doi.org/10.1016/j.earscirev.2009.10.002.

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32

Hoernle, K., J. White, P. van den Bogaard, et al. "Lithospheric removal: The cause of widespread Cenozoic intraplate volcanism on Zealandia?" Geochimica et Cosmochimica Acta 70, no. 18 (2006): A256. http://dx.doi.org/10.1016/j.gca.2006.06.514.

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33

Fourré, Elise, Patrick Allard, Philippe Jean-Baptiste, Dario Cellura, and Francesco Parello. "H3e/H4e Ratio in Olivines from Linosa, Ustica, and Pantelleria Islands (Southern Italy)." Journal of Geological Research 2012 (March 1, 2012): 1–8. http://dx.doi.org/10.1155/2012/723839.

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We report helium isotope data for 0.03–1 Ma olivine-bearing basaltic hawaiites from three volcanoes of the southern Italy magmatic province (Ustica, Pantelleria, and Linosa Islands). Homogenous H3e/H4e ratios (range: 7.3–7.6 Ra) for the three islands, and their similarity with the ratio of modern volcanic gases on Pantelleria, indicate a common magmatic end-member. In particular, Ustica (7.6±0.2 Ra) clearly differs from the nearby Aeolian Islands Arc volcanism, despite its location on the Tyrrhenian side of the plate boundary. Although limited in size, our data set complements the large existi

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34

Zhang, Maoliang, Zhengfu Guo, Zhihui Cheng, Lihong Zhang, and Jiaqi Liu. "Late Cenozoic intraplate volcanism in Changbai volcanic field, on the border of China and North Korea: insights into deep subduction of the Pacific slab and intraplate volcanism." Journal of the Geological Society 172, no. 5 (2014): 648–63. http://dx.doi.org/10.1144/jgs2014-080.

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35

Ryazantsev, A. V., A. V. Pilitsina, I. A. Novikov, and K. E. Degtyarev. "CARBONIFEROUS 40Ar/39Ar AGE OF THE RARE METAL-ENRICHED RHYOLITES AND IGNIMBRITES IN THE SAKMARA ALLOCHTHON OF THE SOUTHERN URALS, THEIR GEOCHEMICAL FEATURES AND GEODYNAMIC SETTING." Proceedings of higher educational establishments. Geology and Exploration, no. 3 (June 25, 2018): 23–32. http://dx.doi.org/10.32454/0016-7762-2018-3-23-32.

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In the structure of the Sakmara allochthon of the Southern Uralssequence with rhyolites and ignimbrites locally occures. They have Nb-Zr-REE geochemical specialization. This sequence unconformably overlays folded Paleozoic complexes, including the Devonian ones. Rhyolite contains K-feldspar and quartz phenocrysts, K-feldspar glomeroporphyrites and granite xenolith. Geochemical features of the rhyolites show intraplate-originated affinities and A-type granite composition.40Ar/39Ar age of the felsitic matrix of the rhyolites of 303±2 Ma defines the age of the volcanic complex origin. For feldspa

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36

Rasskazov, S. V., A. V. Rybin, A. V. Degterev, I. S. Chuvashova, T. A. Yasnygina, and E. V. Saranina. "Pliocene adakite-like accent of andesites and dacites from the Orlov volcanic field (Sakhalin Island)." Geosystems of Transition Zones 5, no. 3 (2021): 255–74. http://dx.doi.org/10.30730/gtrz.2021.5.3.255-274.

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Adakite-like geochemical signature (high Sr/Y ratio at a low Y concentration) is recognized in andesites and dacites, associated with intraplate basalts in the Orlov volcanic field of Sakhalin Island. These rocks denote the final (Pliocene) accent of intraplate volcanism in the Lesogorsk zone, which began in the Middle Miocene in an area of its junction with the Chekhov zone of the preceded (Oligocene-Early Miocene) suprasubduction one. The adakite-like accent was related to the Sakhalin folding phase that accompanied the general structural reorganization in the back-side region in the Japan a

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37

Manjón-Cabeza Córdoba, Antonio, and Maxim D. Ballmer. "The role of edge-driven convection in the generation of volcanism – Part 1: A 2D systematic study." Solid Earth 12, no. 3 (2021): 613–32. http://dx.doi.org/10.5194/se-12-613-2021.

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Abstract. The origin of intraplate volcanism is not explained by plate tectonic theory, and several models have been put forward for explanation. One of these models involves edge-driven convection (EDC), in which cold and thick continental lithosphere is juxtaposed with warm and thin oceanic lithosphere to trigger convective instability. To test whether EDC can produce long-lived high-volume magmatism, we run numerical models of EDC for a wide range of mantle properties and edge (i.e., the oceanic–continental transition) geometries. We find that the most important parameters that govern EDC a

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38

Bianchini, G., L. Beccaluva, and F. Siena. "Post-collisional and intraplate Cenozoic volcanism in the rifted Apennines/Adriatic domain." Lithos 101, no. 1-2 (2008): 125–40. http://dx.doi.org/10.1016/j.lithos.2007.07.011.

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39

Wei, Wei, Jiandong Xu, Dapeng Zhao, and Yaolin Shi. "East Asia mantle tomography: New insight into plate subduction and intraplate volcanism." Journal of Asian Earth Sciences 60 (October 2012): 88–103. http://dx.doi.org/10.1016/j.jseaes.2012.08.001.

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40

Shaw, J. E., J. A. Baker, A. J. R. Kent, K. M. Ibrahim, and M. A. Menzies. "The Geochemistry of the Arabian Lithospheric Mantle--a Source for Intraplate Volcanism?" Journal of Petrology 48, no. 8 (2007): 1495–512. http://dx.doi.org/10.1093/petrology/egm027.

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41

Wessel, P. "Sizes and Ages of Seamounts Using Remote Sensing: Implications for Intraplate Volcanism." Science 277, no. 5327 (1997): 802–5. http://dx.doi.org/10.1126/science.277.5327.802.

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42

Zhao, Dapeng, and You Tian. "Changbai intraplate volcanism and deep earthquakes in East Asia: a possible link?" Geophysical Journal International 195, no. 2 (2013): 706–24. http://dx.doi.org/10.1093/gji/ggt289.

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43

Giannerini, G., R. Campredon, G. Feraud, and B. Abou Zakhem. "Deformations intraplaques et volcanisme associe; exemple de la bordure NW de la plaque Arabique au Cenozoique." Bulletin de la Société Géologique de France IV, no. 6 (1988): 937–47. http://dx.doi.org/10.2113/gssgfbull.iv.6.937.

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44

Stelten, Mark E., Drew T. Downs, Duane E. Champion, et al. "The timing and compositional evolution of volcanism within northern Harrat Rahat, Kingdom of Saudi Arabia." GSA Bulletin 132, no. 7-8 (2019): 1381–403. http://dx.doi.org/10.1130/b35337.1.

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Abstract Harrat Rahat, one of several large, basalt-dominated volcanic fields in western Saudi Arabia, is a prime example of continental, intraplate volcanism. Excellent exposure makes this an outstanding site to investigate changing volcanic flux and composition through time. We present 93 40Ar/39Ar ages and six 36Cl surface-exposure ages for volcanic deposits throughout northern Harrat Rahat that, when integrated with a new geologic map, define 12 eruptive stages. Exposed volcanic deposits in the study area erupted &lt;1.2 Ma, and 214 of 234 eruptions occurred &lt;570 ka. Two eruptio

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45

Phillips, Thomas B., and Craig Magee. "Structural controls on the location, geometry and longevity of an intraplate volcanic system: the Tuatara Volcanic Field, Great South Basin, New Zealand." Journal of the Geological Society 177, no. 5 (2020): 1039–56. http://dx.doi.org/10.1144/jgs2020-050.

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Intraplate volcanism is widely distributed across the continents, but the controls on the 3D geometry and longevity of individual volcanic systems remain poorly understood. Geophysical data provide insights into magma plumbing systems, but, as a result of the relatively low resolution of these techniques, it is difficult to evaluate how magma transits highly heterogeneous continental interiors. We use borehole-constrained 2D seismic reflection data to characterize the 3D geometry of the Tuatara Volcanic Field located offshore New Zealand's South Island and investigate its relationship with the

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46

Aydar, E., A. Gourgaud, C. Deniel, N. Lyberis, and N. Gundogdu. "Le volcanisme quaternaire d'Anatolie centrale (Turquie): association de magmatismes calco-alcalin et alcalin en domaine de convergence." Canadian Journal of Earth Sciences 32, no. 7 (1995): 1058–69. http://dx.doi.org/10.1139/e95-087.

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Collision volcanism in Central Anatolia (Cappadocia) began at least in the late Miocene. Because of the North–South Arabian-Eurasian convergence since this period, the Anatolian block is displaced towards the West along the North and East Anatolian strike-slip faults. Kinematic reconstructions show that the East Anatolian Fault is both sinistral and convergent. As a consequence, the Anatolian block is currently being deformed. Quaternary volcanism in Central Anatolia is represented by several hundreds of monogenetic scoria cones, lava flows, maars, and domes as well as two strato-volcanoes, Ha

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47

Panter, Kurt Samuel. "Chapter 1.3 Antarctic volcanism: petrology and tectonomagmatic overview." Geological Society, London, Memoirs 55, no. 1 (2021): 43–53. http://dx.doi.org/10.1144/m55-2020-10.

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AbstractPetrological investigations over the past 30 years have significantly advanced our knowledge of the origin and evolution of magmas emplaced within and erupted on top of the Antarctic Plate. Over the last 200 myr Antarctica has experienced: (1) several episodes of rifting, leading to the fragmentation of Gondwana and the formation byc.83 Ma of the current Antarctica Plate; (2) long-lived subduction that shut down progressively eastwards along the Gondwana margin in the Late Cretaceous and is still active at the northernmost tip of the Antarctic Peninsula; and (3) broad extension across

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48

Baker, Joel, Gilles Chazot, Martin Menzies, and Matthew Thirlwall. "Metasomatism of the shallow mantle beneath Yemen by the Afar plume—Implications for mantle plumes, flood volcanism, and intraplate volcanism." Geology 26, no. 5 (1998): 431. http://dx.doi.org/10.1130/0091-7613(1998)026<0431:motsmb>2.3.co;2.

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49

ZHAO, Dapeng. "Origin of the Changbai intraplate volcanism in Northeast China: Evidence from seismic tomography." Chinese Science Bulletin 49, no. 13 (2004): 1401. http://dx.doi.org/10.1360/04wd0125.

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50

Cohen, B. E., P. M. Vasconcelos, and K. M. Knesel. "40Ar/39Ar constraints on the timing of Oligocene intraplate volcanism in southeast Queensland ∗." Australian Journal of Earth Sciences 54, no. 1 (2007): 105–25. http://dx.doi.org/10.1080/08120090600981483.

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