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Influence of permeability on hydrothermal circulation in the sediment-buried oceanic crust

Influence of permeability on hydrothermal circulation in the sediment-buried oceanic crust

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_wanfang_journals_zgkx_ed200607011

Influence of permeability on hydrothermal circulation in the sediment-buried oceanic crust

About this item

Full title

Influence of permeability on hydrothermal circulation in the sediment-buried oceanic crust

Publisher

Dordrecht: Springer Nature B.V

Journal title

Science China. Earth sciences, 2006-07, Vol.49 (7), p.773-784

Language

English

Formats

Publication information

Publisher

Dordrecht: Springer Nature B.V

More information

Scope and Contents

Contents

Hydrothermal convection in the upper oceanic crust has been inferred to be a common and important process. Under the simplified conditions of planar boundaries, permeability provides a strong constraint on the pattern of circulation, the dimensions of convective cells and flow field of hydrothermal circulation. By applying an advanced numerical mod...

Alternative Titles

Full title

Influence of permeability on hydrothermal circulation in the sediment-buried oceanic crust

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_wanfang_journals_zgkx_ed200607011

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_wanfang_journals_zgkx_ed200607011

Other Identifiers

ISSN

1674-7313,1006-9313

E-ISSN

1869-1897,1862-2801

DOI

10.1007/s11430-006-0773-y

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