Melting of dehydrated oceanic crust from the stagnant slab and of the hydrated mantle transition zone: Constraints from Cenozoic alkaline basalts in eastern China

Tetsuya Sakuyama, Wei Tian, Jun Ichi Kimura, Yoshio Fukao, Yuka Hirahara, Toshiro Takahashi, Ryoko Senda, Qing Chang, Takashi Miyazaki, Masayuki Obayashi, Hiroshi Kawabata, Yoshiyuki Tatsumi

研究成果: ジャーナルへの寄稿記事

75 引用 (Scopus)

抄録

The feasibility of oceanic igneous crust melting in stagnant slabs has previously been proposed from experimental petrological research. However, geochemical evidence for such melting has not yet been found from igneous rocks. We present evidence to suggest that melts from the igneous layer in the stagnant Pacific slab contributed to the source composition of basalts erupted in eastern China. Fe-rich (> 13 wt%), Si-poor (< 43 wt%) basalts occur only above the leading edge of the stagnant Pacific slab in eastern China, ~. 2000. km west of the Pacific Plate trench. The source of these basalts has Nd-Hf and Sr-Nd-Pb isotopic compositions akin to those of the igneous layer in the Pacific slab, and their extremely low Rb and Pb contents suggest that their source material was modified by subduction processes. Together with forward modeling calculation on trace elements and isotope compositions, these geochemical characteristics imply that they received a contribution from fluid released from hydrated transition zone and dehydrated carbonate-bearing oceanic crust in the stagnant slab, without a long time-integrated ingrowth of Sr-Nd-Hf-Pb isotope systems, almost at the leading edge of the stagnant Pacific slab.

元の言語英語
ページ(範囲)32-48
ページ数17
ジャーナルChemical Geology
359
DOI
出版物ステータス出版済み - 11 14 2013

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transition zone
oceanic crust
slab
Melting
melting
basalt
mantle
Isotopes
Bearings (structural)
Chemical analysis
Igneous rocks
Carbonates
Trace Elements
isotope
Fluids
forward modeling
Pacific plate
igneous rock
trench
isotopic composition

All Science Journal Classification (ASJC) codes

  • Geology
  • Geochemistry and Petrology

これを引用

Melting of dehydrated oceanic crust from the stagnant slab and of the hydrated mantle transition zone : Constraints from Cenozoic alkaline basalts in eastern China. / Sakuyama, Tetsuya; Tian, Wei; Kimura, Jun Ichi; Fukao, Yoshio; Hirahara, Yuka; Takahashi, Toshiro; Senda, Ryoko; Chang, Qing; Miyazaki, Takashi; Obayashi, Masayuki; Kawabata, Hiroshi; Tatsumi, Yoshiyuki.

:: Chemical Geology, 巻 359, 14.11.2013, p. 32-48.

研究成果: ジャーナルへの寄稿記事

Sakuyama, T, Tian, W, Kimura, JI, Fukao, Y, Hirahara, Y, Takahashi, T, Senda, R, Chang, Q, Miyazaki, T, Obayashi, M, Kawabata, H & Tatsumi, Y 2013, 'Melting of dehydrated oceanic crust from the stagnant slab and of the hydrated mantle transition zone: Constraints from Cenozoic alkaline basalts in eastern China', Chemical Geology, 巻. 359, pp. 32-48. https://doi.org/10.1016/j.chemgeo.2013.09.012
Sakuyama, Tetsuya ; Tian, Wei ; Kimura, Jun Ichi ; Fukao, Yoshio ; Hirahara, Yuka ; Takahashi, Toshiro ; Senda, Ryoko ; Chang, Qing ; Miyazaki, Takashi ; Obayashi, Masayuki ; Kawabata, Hiroshi ; Tatsumi, Yoshiyuki. / Melting of dehydrated oceanic crust from the stagnant slab and of the hydrated mantle transition zone : Constraints from Cenozoic alkaline basalts in eastern China. :: Chemical Geology. 2013 ; 巻 359. pp. 32-48.
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abstract = "The feasibility of oceanic igneous crust melting in stagnant slabs has previously been proposed from experimental petrological research. However, geochemical evidence for such melting has not yet been found from igneous rocks. We present evidence to suggest that melts from the igneous layer in the stagnant Pacific slab contributed to the source composition of basalts erupted in eastern China. Fe-rich (> 13 wt{\%}), Si-poor (< 43 wt{\%}) basalts occur only above the leading edge of the stagnant Pacific slab in eastern China, ~. 2000. km west of the Pacific Plate trench. The source of these basalts has Nd-Hf and Sr-Nd-Pb isotopic compositions akin to those of the igneous layer in the Pacific slab, and their extremely low Rb and Pb contents suggest that their source material was modified by subduction processes. Together with forward modeling calculation on trace elements and isotope compositions, these geochemical characteristics imply that they received a contribution from fluid released from hydrated transition zone and dehydrated carbonate-bearing oceanic crust in the stagnant slab, without a long time-integrated ingrowth of Sr-Nd-Hf-Pb isotope systems, almost at the leading edge of the stagnant Pacific slab.",
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AU - Senda, Ryoko

AU - Chang, Qing

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AU - Tatsumi, Yoshiyuki

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