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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 (May 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 (May 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 (September 26, 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 (February 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 (August 6, 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 series of geodynamic models from 62 to 42 Ma in which the plates are driven by the attached subducting slabs and mantle drag/suction forces. We compare our modelled intraplate deformation history with those types of intraplate volcanism that lack a clear age progression. Our models suggest that changes in Cenozoic subduction zone topology caused intraplate deformation to trigger volcanism along several linear seafloor structures, mostly by reactivation of existing seamount chains, but occasionally creating new volcanic chains on crust weakened by fracture zones and extinct ridges. Around 55 Ma, subduction of the Pacific-Izanagi ridge reconfigured the major tectonic forces acting on the plate by replacing ridge push with slab pull along its northwestern perimeter, causing lithospheric extension along pre-existing weaknesses. Large-scale deformation observed in the models coincides with the seamount chains of Hawaii, Louisville, Tokelau and Gilbert during our modelled time period of 62 to 42 Ma. We suggest that extensional stresses between 72 and 52 Ma are the likely cause of large parts of the formation of the Gilbert chain and that localised extension between 62 and 42 Ma could cause late-stage volcanism along the Musicians volcanic ridges. Our models demonstrate that early Cenozoic changes in Pacific plate driving forces only cause relatively minor changes in Pacific absolute plate motion directions, and cannot be responsible for the Hawaiian–Emperor bend (HEB), confirming previous interpretations that the 47 Ma HEB does not primarily reflect an absolute plate motion event.

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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 (January 14, 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 series of geodynamic models from 62 to 42 Ma in which the plates are driven by the attached subducting slabs and mantle drag/suction forces. We compare our modelled intraplate deformation history with those types of intraplate volcanism that lack a clear age progression. Our models suggest that changes in Cenozoic subduction zone topology caused intraplate deformation to trigger volcanism along several linear seafloor structures, mostly by reactivation of existing seamount chains, but occasionally creating new volcanic chains on crust weakened by fracture zones and extinct ridges. Around 55 Ma subduction of the Pacific-Izanagi ridge reconfigured the major tectonic forces acting on the plate by replacing ridge push with slab pull along its north-western perimeter, causing lithospheric extension along pre-existing weaknesses. Large scale deformation observed in the models coincides with the seamount chains of Hawaii, Louisville, Tokelau, and Gilbert during our modelled time period of 62 to 42 Ma. We suggest that extensional stresses between 72 and 52 Ma are the likely cause of large parts of the formation of the Gilbert chain and that localised extension between 62 and 42 Ma could cause late-stage volcanism along the Musicians Volcanic Ridges. Our models demonstrate that early Cenozoic changes in Pacific plate driving forces only cause relatively minor changes in Pacific absolute plate motions, and cannot be responsible for the Hawaii-Emperor Bend (HEB), confirming previous interpretations that the 47 Ma HEB does not reflect an absolute plate motion event.

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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 (December 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 [>1 billion years (Ga) old] in the slab-poor south, from a northern EM1/EM2 reservoir, reflecting a more recent voluminous influx of oceanic lithosphere into the mantle transition zone. We provide a unified theory linking plate boundary and slab volume reconstructions to upper mantle reservoirs and intraplate volcano geochemistry.

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8

Leeman, William P. "Intraplate volcanism in eastern Australia and New Zealand." Geochimica et Cosmochimica Acta 61, no. 10 (May 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 (March 20, 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 (March 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 (June 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 (January 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, Janne Blichert-Toft, F. Hauff, James B. Gill, and Hans-Ulrich Schmincke. "Hafnium isotopic variations in East Atlantic intraplate volcanism." Contributions to Mineralogy and Petrology 162, no. 1 (September 19, 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 (June 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 (January 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 Golfo de California, y fallas de tipo "basin-and-range" (extensional) al norte del CVM.La zona de debilidad fijó el lugar y la orientación del CVM. Posteriormente, en correspondencia con la cesación de subducción por la Costa de la América del Norte a la parte norte de la zona, se desarrollaron tectónicos extensionales. Al sur, por donde la subducción tipo chileno prevalecía, no fue posible el tectonismo extensional. De este modo, la zona de debilidad llego a ser un cinturón de acomodación, quizás asociado con extensión interna, entre regiones de kinemáticos estructurales contrastantes. En breve, llegó a ser un transforme de tipo intraplaca (con fuga) [en el sentido de Davis, 1980], por donde fue posible y se localizó el volcanismo. Paradójicamente, esta interpretación implica que el volcanismo a lo largo del CVM está más aliado a la cesación de la subducción al norte del CVM Que a la subducción continua hacia el Sur. También da a entender que el CVM es fundamentalmente diferente de los arcos volcánicos típicos del borde pacífico.

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17

Yang, Jianfeng, and Manuele Faccenda. "Intraplate volcanism originating from upwelling hydrous mantle transition zone." Nature 579, no. 7797 (February 26, 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 (December 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 (October 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 (April 16, 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 (May 23, 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 magmatic pulses at ca. 141, ca. 137, and ca. 130 Ma as defined by the age peaks. Zircon Hf isotopic data show markedly negative εHf(t) values of –23.0 to –11.8, and corresponding Hf crustal model ages (TDMC) are in the range of ca. 2650 to 1944 Ma, suggesting magma derivation through melting of Paleoproterozoic crustal materials with minor input of reworked Neoarchean components. Geochemically, the rhyolitic rocks correspond to A-type granites, with a mixed arc- and subduction-related signature, although generated in an extensional intraplate setting through partial melting of the mafic lower crust and upper crustal fractional crystallization. We correlate the late Mesozoic intraplate volcanism to the westward subduction of the Paleo-Pacific Plate and its far-field effect. Lithospheric extension and slab rollback of the Paleo-Pacific Plate are considered as the main triggers for the multiple eruptions. The late Mesozoic volcanism in the study area and adjacent regions also broadly coincide with the tectonic transition from the Paleozoic Paleo-Asian to Mesozoic Paleo-Pacific subduction realm with concomitant compressional to extensional tectonic regime.

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22

Mukhopadhyay, Ranadhir. "Post-Cretaceous intraplate volcanism in the Central Indian Ocean Basin." Marine Geology 151, no. 1-4 (October 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 (October 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 (August 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 peralkaline, silicic volcanics.

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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 (December 11, 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 Ocean to depths of 1000 km. Such anomalies correlate with the heat flow anomalies and are thus indica‐ tive of a deep source. The absence of deep roots in the western part of the profile from the Caspian to the Western Mediterranean suggests lateral extension of the anomalously ‘hot’ mantle from the Afar branch of the African super‐ plume. The groups of volcanic formations in the Baikal region and the Far East are spatially associated with heat flow anomalies that are three times higher than the background values. A correlation between intraplate volcanism and the lithosphere conductivity suggests the presence of positive anomalies in all volcanic clusters, despite the fact that their background values are considerably different. In the continental part, velocity anomalies are typical of all volcanic groups with positive conductivity anomalies. It is evidenced by seismic tomography that all the volcanic groups (ex‐ cept the Alpine‐Caucasian) have ‘hot’ roots in the upper mantle to depths of 1200 km. The highest maximum conduc‐ tivity values are typical of the zones wherein high intraplate seismicity is absent. Along the profile, there are several zones of high intraplate seismicity, which are separated by aseismic zones or plate boundaries. This suggest the influ‐ ence of the heated state of the mantle and the occurrence of zones of increased conductivity in the lithosphere.

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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 (January 28, 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 (November 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, F. Hauff, D. S. Coombs, R. Werner, C. Timm, D. Garbe-Schönberg, A. Reay, and A. F. Cooper. "Cenozoic intraplate volcanism on New Zealand: Upwelling induced by lithospheric removal." Earth and Planetary Science Letters 248, no. 1-2 (August 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, Folkmar Hauff, Paul van den Bogaard, James White, Nick Mortimer, and Dieter Garbe-Schönberg. "Temporal and geochemical evolution of the Cenozoic intraplate volcanism of Zealandia." Earth-Science Reviews 98, no. 1-2 (January 1, 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, F. Hauff, D. Coombs, R. Werner, C. Timm, D. Garbe-Schönberg, A. Reay, and A. Cooper. "Lithospheric removal: The cause of widespread Cenozoic intraplate volcanism on Zealandia?" Geochimica et Cosmochimica Acta 70, no. 18 (August 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 existing database for helium isotope in southern Italy and adds further constraints upon the spatial extent of intraplate alkaline volcanism in southern Mediterranea. As already discussed by others, the He-Pb isotopic signature of this magmatic province indicates a derivation from a mantle diapir of a OIB-type that is partially diluted by the depleted upper mantle (MORB mantle) at its periphery.

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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 (December 15, 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 feldspar phenocrysts the age of 306±3 Ma and 337±3 Ma is obtained. The first value coincides to the matrix age and connected with formation of the volcanic complex. The second value belongs, apparently, to xenogenic material. Obtained age values reflect the evolution of Carboniferous active continental margin magmatism, widespread in different structural zones of the Urals. Rare-metal rhyolites characterize the final late Carboniferous intraplate (rift-related) back-arc magmatism at the active continental margin. Volcanism preceded to a collision-related ophiolitic thrust nappes emplacement.

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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 arc system. Such a geological environment differed from the one of classical adakites generation resulted from melting of a young slab in the Aleutian island arc. It is supposed, that the Sakhalin adakite-like magmas were produced in deep-seated sources of the crust-mantle transition displayed in the Sakhalin-Hokkaido-Japan Sea zone of hot transtension due to drastic change of tectonic deformations from the thin crust of the South Tatar Basin to the thicker one of its northeastern extremity.

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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 (March 10, 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 are the rheological parameters mantle viscosity η0 and activation energy Ea. However, even the maximum melting volumes predicted by our most extreme cases are insufficient to account for island-building volcanism on old seafloor, such as at the Canary Islands and Cabo Verde. Also, beneath old seafloor, localized EDC-related melting commonly transitions into widespread melting due to small-scale sublithospheric convection, inconsistent with the distribution of volcanism at these volcano chains. In turn, EDC is a good candidate to sustain the formation of small seamounts on young seafloor, as it is a highly transient phenomenon that occurs in all our models soon after initiation. In a companion paper, we investigate the implications of interaction of EDC with mantle plume activity (Manjón-Cabeza Córdoba and Ballmer, 2021).

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Bianchini, G., L. Beccaluva, and F. Siena. "Post-collisional and intraplate Cenozoic volcanism in the rifted Apennines/Adriatic domain." Lithos 101, no. 1-2 (February 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 (June 7, 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 (August 8, 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 (August 16, 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 (November 1, 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, Hannah R. Dietterich, Andrew T. Calvert, Thomas W. Sisson, Gail A. Mahood, and Hani Zahran. "The timing and compositional evolution of volcanism within northern Harrat Rahat, Kingdom of Saudi Arabia." GSA Bulletin 132, no. 7-8 (November 4, 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 <1.2 Ma, and 214 of 234 eruptions occurred <570 ka. Two eruptions occurred in the Holocene, including a historically described basalt eruption in 1256 C.E. and a trachyte eruption newly recognized as Holocene (4.2 ± 5.2 ka). An estimated ∼82 km3 (dense rock equivalent) of volcanic product have erupted since 1.2 Ma, though this is a lower limit due to concealment of deposits >570 ka. Over the past 570 k.y., the average eruption rate was 0.14 km3/k.y., but volcanism was episodic with periods alternating between low (0.04–0.06 km3/k.y.) and high (0.1–0.3 km3/k.y.) effusion rates. Before 180 ka, eruptions vented from the volcanic field’s dominant eastern vent axis and from a subsidiary, diffuse, western vent axis. After 180 ka, volcanism focused along the eastern vent axis, and the composition of volcanism varied systematically along its length from basalt dominated in the north to trachyte dominated in the south. We hypothesize that these compositional variations <180 ka reflect the growth of a mafic intrusive complex beneath the southern portion of the vent axis, which led to the development of evolved magmas.

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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 (June 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 pre-existing structure. This c. 270 km2 field is dominated by a dome-shaped lava edifice, surrounded and overlain by c. 69 volcanoes and >70 sills emplaced over 40 myr from the Late Cretaceous to Early Eocene (c. 85–45 Ma). The Tuatara Volcanic Field is located above a basement terrane boundary represented by the Livingstone Fault; the recently active Auckland Volcanic Field is similarly located along-strike on North Island. We suggest that the Livingstone Fault controlled the location of the Tuatara Volcanic Field by producing relief at the base of the lithosphere, thereby focussing lithospheric detachment over c. 40 myr, and provided a pathway that facilitated the ascent of magma. We highlight how observations from ancient intraplate volcanic systems may inform our understanding of active intraplate volcanic systems, including the Auckland Volcanic Field.Supplementary material: Interpreted seismic section showing well control on stratigraphic interpretation is available at https://doi.org/10.6084/m9.figshare.c.5004464

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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 (July 1, 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, Hasan Dag and Erciyes Dag. The monogenetic volcanism is bimodal (basalts and rhyolites), whereas the stratovolcanoes exhibit a complete calc-alkaline suite, from basalts to rhyolites. Most of the igneous products are calc-alkaline. Basalts erupted mainly from the monogenetic cones, lava flows, and maars. Andesites are encountered in the strato-volcanoes as lava flows, domes, and nuees ardentes deposits. Dacites and rhyolites occur as ignimbrites and dispersed maars and domes. Volcanic events were recorded up to historical times. Some basalts from monogenetic edifices, contemporaneous with the calc-alkaline suite, exhibit mineralogical and geochemical features that are typical of intraplate alkaline suites, such as normative nepheline, alkali feldspars, and Ti and Cr-rich Cpx. Euhedral microlites of aluminous garnet, although rare, have been observed in basalts, rhyodacites, and rhyolites. This association of contemporaneous calc-alkaline and alkaline suites may be related to collision tectonics.

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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 West Antarctica that produced one of the Earth's major continental rift systems. The dynamic tectonic history of Antarctica since the Triassic has led to a diversity of volcano types and igneous rock compositions with correspondingly diverse origins. Many intriguing questions remain about the petrology of mantle sources and the mechanisms for melting during each tectonomagmatic phase. For intraplate magmatism, the upwelling of deep mantle plumes is often evoked. Alternatively, subduction-related metasomatized mantle sources and melting by more passive means (e.g. edge-driven flow, translithospheric faulting, slab windows) are proposed. A brief review of these often competing models is provided in this chapter along with recommendations for ongoing petrological research in Antarctica.

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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 (February 2007): 105–25. http://dx.doi.org/10.1080/08120090600981483.

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