DOI: 10.1016/j.epsl.2018.02.039
Scopus记录号: 2-s2.0-85046035202
论文题名: Subducted slab-plume interaction traced by magnesium isotopes in the northern margin of the Tarim Large Igneous Province
作者: Cheng Z. ; Zhang Z. ; Xie Q. ; Hou T. ; Ke S.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2018
卷: 489 起始页码: 100
结束页码: 110
语种: 英语
英文关键词: ferrobasalt
; mantle plume
; Mg isotopes
; subducted slab
; Tarim Large Igneous Province
Scopus关键词: Basalt
; Calcite
; Iron oxides
; Isotopes
; Magnesia
; Magnesite
; Sedimentary rocks
; Tectonics
; Thermal plumes
; ferrobasalt
; Mantle plume
; Mg isotopes
; subducted slab
; Tarim large igneous provinces
; Magnesium
; basalt
; igneous geochemistry
; isotopic composition
; large igneous province
; magma
; magnesium
; mantle plume
; slab
; subduction
英文摘要: Incorporation of subducted slabs may account for the geochemical and isotopic variations of large igneous provinces (LIPs). However, the mechanism and process by which subducted slabs are involved into magmas is still highly debated. Here, we report a set of high resolution Mg isotopes for a suite of alkaline and Fe-rich rocks (including basalts, mafic–ultramafic layered intrusions, diabase dykes and mantle xenoliths in the kimberlitic rocks) from Tarim Large Igneous Province (TLIP). We observed that δ26Mg values of basalts range from −0.29 to −0.45‰ −0.31 to −0.42‰ for mafic–ultramafic layered intrusions, −0.28 to −0.31‰ for diabase dykes and −0.29 to −0.44‰ for pyroxenite xenoliths from the kimberlitic rocks, typically lighter than the normal mantle source (−0.25‰±0.04, 2 SD). After carefully precluding other possibilities, we propose that the light Mg isotopic compositions and high FeO contents should be ascribed to the involvement of recycled sedimentary carbonate rocks and pyroxenite/eclogite. Moreover, from basalts, through layered intrusions to diabase dykes, (87Sr/86Sr)i values and δ18OV-SMOW declined, whereas ε(Nd)t and δ26Mg values increased with progressive partial melting of mantle, indicating that components of carbonate rock and pyroxenite/eclogite in the mantle sources were waning over time. In combination with the previous reported Mg isotopes for carbonatite, nephelinite and kimberlitic rocks in TLIP, two distinct mantle domains are recognized for this province: 1) a lithospheric mantle source for basalts and mafic–ultramafic layered intrusions which were modified by calcite/dolomite and eclogite-derived high-Si melts, as evidenced by enriched Sr–Nd–O and light Mg isotopic compositions; 2) a plume source for carbonatite, nephelinite and kimberlitic rocks which were related to magnesite or periclase/perovskite involvement as reflected by depleted Sr–Nd–O and extremely light Mg isotopes. Ultimately, our study suggests that subducted slabs could make important contributions to LIP generation, and establishes a potential linkage between plate tectonics and mantle plume. © 2018 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109967
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 100083, China; Institut für Mineralogie, Leibniz Universität Hannover, Callinstraße 3, Hannover, D-30167, Germany
Recommended Citation:
Cheng Z.,Zhang Z.,Xie Q.,et al. Subducted slab-plume interaction traced by magnesium isotopes in the northern margin of the Tarim Large Igneous Province[J]. Earth and Planetary Science Letters,2018-01-01,489