中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Magma-Mush Interactions in the Lower Oceanic Crust: Insights From Atlantis Bank Layered Series (Southwest Indian Ridge)

文献类型:期刊论文

作者Boulanger, M.1,7; France, L.1; Ferrando, C.1,6; Ildefonse, B.5; Ghosh, B.4; Sanfilippo, A.6; Liu, C. -Z.3; Morishita, T.2; Koepke, J.7; Bruguier, O.5
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2021-09-01
卷号126期号:9页码:29
关键词crystal mush lower oceanic crust magmatic flow magma intrusion reactive porous flow assimilation-fractional crystallization
ISSN号2169-9313
DOI10.1029/2021JB022331
英文摘要Magma migration and differentiation processes are key to understanding the development and evolution of oceanic magma reservoirs. To provide new quantitative geochemical constraints on these processes, we applied a high-resolution approach to study an interlayered section of the lower oceanic crust sampled at Atlantis Bank, on the (ultra)slow-spreading Southwest Indian Ridge. The section is characterized by sharp grain-size layering between fine- and coarse-grained olivine gabbros that is representative of other layered structures described at the Atlantis Bank oceanic core complex. The textures and fabrics of the layers and the nature of their contacts indicate formation by intrusion of a magma (i.e., crystal-bearing) into an almost solidified coarse-grained mush. Petrographic observations and in situ incompatible trace element signatures indicate that the fine- and coarse-grained layers record reactive porous migration of melts. Widespread reactive porous flow occurred prior to intrusion within the coarse-grained gabbro, producing mineral compositions enriched in incompatible elements. The intrusive fine-grained lithology records a late stage event of localized reactive melt percolation in cm-scale structures, which lead to strong light rare earth elements depletion relative to heavy rare earth elements. In addition, we highlight the occurrence of interactions at the contacts between layers and partial modification in compositions of the intruded lithology. This layered section likely represents a contact between two larger magma bodies emplaced within the lower crust during accretion, where the type of melt migration (intrusion or porous flow) and the modalities of melt percolation (widespread or localized) strongly govern the composition of the crustal lithologies.
WOS关键词TRACE-ELEMENT ; CORE COMPLEXES ; GABBRO ; CRYSTALLIZATION ; CONSTRAINTS ; LITHOSPHERE ; CHAMBER ; BENEATH ; ORIGIN ; ASSIMILATION
资助项目CNRS-INSU ; IODP-France ; French Ministry of Research (MESRI) ; Projekt DEAL
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000703087900054
出版者AMER GEOPHYSICAL UNION
资助机构CNRS-INSU ; CNRS-INSU ; IODP-France ; IODP-France ; French Ministry of Research (MESRI) ; French Ministry of Research (MESRI) ; Projekt DEAL ; Projekt DEAL ; CNRS-INSU ; CNRS-INSU ; IODP-France ; IODP-France ; French Ministry of Research (MESRI) ; French Ministry of Research (MESRI) ; Projekt DEAL ; Projekt DEAL ; CNRS-INSU ; CNRS-INSU ; IODP-France ; IODP-France ; French Ministry of Research (MESRI) ; French Ministry of Research (MESRI) ; Projekt DEAL ; Projekt DEAL ; CNRS-INSU ; CNRS-INSU ; IODP-France ; IODP-France ; French Ministry of Research (MESRI) ; French Ministry of Research (MESRI) ; Projekt DEAL ; Projekt DEAL
源URL[http://ir.iggcas.ac.cn/handle/132A11/102697]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Boulanger, M.
作者单位1.Univ Lorraine, CNRS, CRPG, Nancy, France
2.Kanazawa Univ, Coll Sci & Engn, Kanazawa, Ishikawa, Japan
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
4.Univ Calcutta, Dept Geol, Kolkata, India
5.Univ Montpellier, CNRS, Geosci Montpellier, Montpellier, France
6.Univ Pavia, Dipartimento Sci Terra & Ambiente, Pavia, Italy
7.Leibniz Univ Hannover, Inst Mineral, Hannover, Germany
推荐引用方式
GB/T 7714
Boulanger, M.,France, L.,Ferrando, C.,et al. Magma-Mush Interactions in the Lower Oceanic Crust: Insights From Atlantis Bank Layered Series (Southwest Indian Ridge)[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2021,126(9):29.
APA Boulanger, M..,France, L..,Ferrando, C..,Ildefonse, B..,Ghosh, B..,...&Bruguier, O..(2021).Magma-Mush Interactions in the Lower Oceanic Crust: Insights From Atlantis Bank Layered Series (Southwest Indian Ridge).JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,126(9),29.
MLA Boulanger, M.,et al."Magma-Mush Interactions in the Lower Oceanic Crust: Insights From Atlantis Bank Layered Series (Southwest Indian Ridge)".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 126.9(2021):29.

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来源:地质与地球物理研究所

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