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DOI | 10.1038/NGEO3009 |
Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow | |
Plumper, Oliver1; Botan, Alexandru2,3,4; Los, Catharina5; Liu, Yang1,6; Malthe-Sorenssen, Anders2,3; Jamtveit, Bjorn2,3 | |
2017-09-01 | |
发表期刊 | NATURE GEOSCIENCE
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ISSN | 1752-0894 |
EISSN | 1752-0908 |
出版年 | 2017 |
卷号 | 10期号:9 |
文章类型 | Article |
语种 | 英语 |
国家 | Netherlands; Norway; Germany |
英文摘要 | The transport of fluids through the Earth's crust controls the redistribution of elements to form mineral and hydrocarbon deposits, the release and sequestration of greenhouse gases, and facilitates metamorphic reactions that influence lithospheric rheology. In permeable systems with a well-connected porosity, fluid transport is largely driven by fluid pressure gradients. In less permeable rocks, deformation may induce permeability by creating interconnected heterogeneities, but without these perturbations, mass transport is limited along grain boundaries or relies on transformation processes that self-generate transient fluid pathways. The latter can facilitate large-scale fluid and mass transport in nominally impermeable rocks without large-scale fluid transport pathways. Here, we show that pervasive, fluid-driven metamorphism of crustal igneous rocks is directly coupled to the production of nanoscale porosity. Using multi-dimensional nano-imaging and molecular dynamics simulations, we demonstrate that in feldspar, the most abundant mineral family in the Earth's crust, electrokinetic transport through reaction-induced nanopores (<100 nm) can potentially be significant. This suggests that metamorphic fluid flow and fluid-mediated mineral transformation reactions can be considerably influenced by nanofluidic transport phenomena. |
领域 | 地球科学 ; 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000409229600017 |
WOS关键词 | ORTHOCLASE (001)-WATER ; GRANITIC-ROCKS ; TRANSPORT ; REPLACEMENT ; MECHANISM ; PERMEABILITY ; ALBITIZATION ; TEMPERATURE ; GENERATION ; GRADIENTS |
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/35164 |
专题 | 地球科学 气候变化 |
作者单位 | 1.Univ Utrecht, Dept Earth Sci, Budapestlaan 4, NL-3584CD Utrecht, Netherlands; 2.Univ Oslo, Dept Geosci, PGP, N-0136 Oslo, Norway; 3.Univ Oslo, Dept Phys, PGP, N-0136 Oslo, Norway; 4.Univ Oslo, Ctr Mat Sci & Nanotechnol, N-0318 Oslo, Norway; 5.Univ Bremen, Dept Geosci, Klagenfurter Str 2, D-28359 Bremen, Germany; 6.Univ Utrecht, Debye Inst Nanomat Sci, Princetonpl 1, NL-3584 CC Utrecht, Netherlands |
推荐引用方式 GB/T 7714 | Plumper, Oliver,Botan, Alexandru,Los, Catharina,et al. Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow[J]. NATURE GEOSCIENCE,2017,10(9). |
APA | Plumper, Oliver,Botan, Alexandru,Los, Catharina,Liu, Yang,Malthe-Sorenssen, Anders,&Jamtveit, Bjorn.(2017).Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow.NATURE GEOSCIENCE,10(9). |
MLA | Plumper, Oliver,et al."Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow".NATURE GEOSCIENCE 10.9(2017). |
条目包含的文件 | 条目无相关文件。 |
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