2017
DOI: 10.1016/j.epsl.2017.02.028
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Mantle transition zone-derived EM1 component beneath NE China: Geochemical evidence from Cenozoic potassic basalts

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Cited by 128 publications
(110 citation statements)
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“…Variation in the Sr, Nd, Pb, and Hf isotopic composition of the Huihe nephelinites. Data for Cenozoic basalts in Eastern China are shown for comparison (NE China: Basu et al, ; Chu et al, ; Kuritani et al, ; Liu, Chen, et al, ; Rasskazov et al, ; Sun, Teng, et al, ; Sun et al, ; Wang et al, ; Yan & Zhao, ; Yan et al, ; Zhang et al, ; Zhang et al, ; Zhao et al, ; Zou et al, ; Zou et al, . North China: Basu et al, ; Chen et al, ; Choi et al, ; Guo et al, ; Han et al, ; Ho et al, ; Li, Ma, et al, ; Wang et al, ; Xu et al, ; Yu et al, ; Zeng et al, ; Zhang et al, ; Zhang et al, ; Zou et al, .…”
Section: Whole‐rock Compositions Of the Huihe Nephelinitesmentioning
confidence: 99%
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“…Variation in the Sr, Nd, Pb, and Hf isotopic composition of the Huihe nephelinites. Data for Cenozoic basalts in Eastern China are shown for comparison (NE China: Basu et al, ; Chu et al, ; Kuritani et al, ; Liu, Chen, et al, ; Rasskazov et al, ; Sun, Teng, et al, ; Sun et al, ; Wang et al, ; Yan & Zhao, ; Yan et al, ; Zhang et al, ; Zhang et al, ; Zhao et al, ; Zou et al, ; Zou et al, . North China: Basu et al, ; Chen et al, ; Choi et al, ; Guo et al, ; Han et al, ; Ho et al, ; Li, Ma, et al, ; Wang et al, ; Xu et al, ; Yu et al, ; Zeng et al, ; Zhang et al, ; Zhang et al, ; Zou et al, .…”
Section: Whole‐rock Compositions Of the Huihe Nephelinitesmentioning
confidence: 99%
“…Sedimentary carbonates have extremely light Mg isotopic compositions (δ 26 Mg = −5.57‰ to −0.38‰; Huang, Ke, et al, ; Wombacher et al, ; Young & Galy, ). Light Mg isotopic signatures of basalts have therefore been widely interpreted to reflect contributions from this isotopically light component in the form of recycled carbonates in their mantle sources (e.g., Huang, Li, et al, ; Li et al, ; Wang et al, ; Yang et al, ). Melts with light Mg isotopic signature, but low or moderately low CaO contents, however, cannot be produced by direct partial melting of carbonate‐bearing source rocks (Wang et al, ).…”
Section: Nature Of the Light Mg Isotope Mantle Componentmentioning
confidence: 99%
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“…Low S and P wave velocity anomalies extend from the top of the mantle transition zone, and possibly from the deep mantle, to several of the Cenozoic volcanic centers (e.g., at Changbaishan, Wudalianchi, Halaha; Figure a), suggesting a close relation between the mantle transition zone and the wide‐spread volcanism (Chen et al, ; Huang & Zhao, ; Kimura et al, ; Tang et al, ; Wei et al, ; Zhao, ). Many geochemical studies have further shown that enriched mantle components play an important role in the formation of the magmas, which are thought to derive from the stagnant Pacific slab and/or from ancient subducted slabs (Kimura et al, ; Kuritani et al, , ; Tang et al, ; Wang et al, ; Xu et al, ).…”
Section: Introductionmentioning
confidence: 99%