DOI: 10.1016/j.epsl.2021.116784
论文题名: Electrical conductivity of omphacite and garnet indicates limited deep water recycling by crust subduction
作者: Liu H. ; Zhang K. ; Ingrin J. ; Yang X.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2021
卷: 559 语种: 英语
中文关键词: crust subduction
; deep water recycling
; electrical conductivity
; experimental studies
; omphacite and garnet
英文关键词: Electric conductivity
; Garnets
; Geochemical surveys
; Metamorphic rocks
; Earth's interior
; Electrical conduction
; Electrical conductivity
; Geochemical investigations
; Geophysical surveys
; Hydrous phasis
; Subducting slabs
; Subduction zones
; Water recycling
; crustal structure
; deep water
; electrical conductivity
; experimental study
; garnet
; omphacite
; subduction
英文摘要: It is usually stated that oceanic crust recycling at subduction zones introduces large quantities of water into Earth's interior. However, it remains clouded how much water is recycled to the deep mantle. This is largely due to the challenge in directly sampling, and analyzing the water content of, a deep subducting crust. The subducting crust below ∼30 km depth is dominated by omphacite and garnet in eclogite-facies rocks. Here we have determined the electrical conductivity of omphacite and garnet in representative subduction-related eclogites, each with varying contents of Fe and H2O that are key in electrical conduction. Considering the measured conductivity, the eclogite chemistry by geochemical investigations and the highly resistive property of subducting crusts by geophysical surveys, we demonstrate that, at 70-120 km depths in the subducting crust, the H2O contents of omphacite and garnet are strikingly small, with the maximum value being <400 and <80 ppm in the former and latter, respectively. The very small water contents indicate extremely water-poor conditions, or very low water activity, during the eclogite-facies metamorphism and in the system. This further implies the absence of appreciated amounts of hydrous phases such as amphibole and chlorite in the matrix, because of the strong ability of omphacite and garnet in hosting water as documented in natural samples. We suggest that the recycling of water to the deep mantle by oceanic crust subduction is probably very limited. The results are important for modeling the conductivity of subducting slabs and understanding the deep water circulation. © 2021 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165570
Appears in Collections: 气候变化与战略
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作者单位: State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China; Univ. Lille, CNRS, INRAE, ENSCL, UMR 8207, UMET, Unité Matériaux et Transformations, Lille, F59000, France
Recommended Citation:
Liu H.,Zhang K.,Ingrin J.,et al. Electrical conductivity of omphacite and garnet indicates limited deep water recycling by crust subduction[J]. Earth and Planetary Science Letters,2021-01-01,559