Hybrid shallow on-axis and deep off-axis hydrothermal circulation at fast-spreading ridges

被引:0
|
作者
Jörg Hasenclever
Sonja Theissen-Krah
Lars H. Rüpke
Jason P. Morgan
Karthik Iyer
Sven Petersen
Colin W. Devey
机构
[1] GEOMAR,Department of Geosciences and Centre for Earth Evolution and Dynamics (CEED)
[2] Helmholtz Centre for Ocean Research Kiel,Department of Earth Sciences
[3] Wischhofstraße 1-3,undefined
[4] 24148 Kiel,undefined
[5] Germany,undefined
[6] University of Oslo,undefined
[7] PO Box 1048,undefined
[8] Blindern,undefined
[9] 0316 Oslo,undefined
[10] Norway,undefined
[11] Royal Holloway,undefined
[12] University of London,undefined
[13] Egham,undefined
[14] Surrey TW20 0EX,undefined
[15] UK,undefined
来源
Nature | 2014年 / 508卷
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摘要
High-resolution three-dimensional simulations of hydrothermal flow beneath fast-spreading ridges predict two interacting flow components — shallow on-axis flow and deeper off-axis flow — that merge to feed axial vent sites, reconciling previously incompatible models favouring only one flow component.
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页码:508 / 512
页数:4
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