GSTDTAP  > 气候变化
DOI10.1002/2017GL072893
Global rates of mantle serpentinization and H-2 production at oceanic transform faults in 3-D geodynamic models
Ruepke, Lars H.1; Hasenclever, Joerg1,2
2017-07-16
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2017
卷号44期号:13
文章类型Article
语种英语
国家Germany
英文摘要

Previous studies have estimated that mantle serpentinization reactions generate H-2 at a rate of 10(10)-10(12) mol/yr along the global mid-ocean ridge (MOR) system. Here we present results of 3-D geodynamic simulations that predict rates of additional mantle serpentinization and H-2 production at oceanic transform faults (OTF). We find that the extent and rate of mantle serpentinization increases with OTF length and is maximum at intermediate slip rates of 5 to 10 cm/yr. The additional global OTF-related production of H-2 is found to be between 6.1 and 10.7 x 10(11) mol/yr, which is comparable to the predicted background MOR rate of 4.1-15.0 x 10(11) mol H-2/yr. This points to oceanic transform faults as potential sites of intense fluid-rock interaction, where chemosynthetic life could be sustained by serpentinization reactions.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000406257400030
WOS关键词HYDROTHERMAL SYSTEMS ; SPREADING RATE ; MASS-TRANSFER ; LITHOSPHERE ; COMMUNITIES ; EVOLUTION ; HYDRATION ; CARBON ; RIDGE ; HEAT
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/27791
专题气候变化
作者单位1.GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany;
2.Univ Bremen, Fac Geosci, Bremen, Germany
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GB/T 7714
Ruepke, Lars H.,Hasenclever, Joerg. Global rates of mantle serpentinization and H-2 production at oceanic transform faults in 3-D geodynamic models[J]. GEOPHYSICAL RESEARCH LETTERS,2017,44(13).
APA Ruepke, Lars H.,&Hasenclever, Joerg.(2017).Global rates of mantle serpentinization and H-2 production at oceanic transform faults in 3-D geodynamic models.GEOPHYSICAL RESEARCH LETTERS,44(13).
MLA Ruepke, Lars H.,et al."Global rates of mantle serpentinization and H-2 production at oceanic transform faults in 3-D geodynamic models".GEOPHYSICAL RESEARCH LETTERS 44.13(2017).
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