Log in to save to my catalogue

Ridge subduction, magmatism, and metallogenesis

Ridge subduction, magmatism, and metallogenesis

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2440408871

Ridge subduction, magmatism, and metallogenesis

About this item

Full title

Ridge subduction, magmatism, and metallogenesis

Publisher

Beijing: Science China Press

Journal title

Science China. Earth sciences, 2020-10, Vol.63 (10), p.1499-1518

Language

English

Formats

Publication information

Publisher

Beijing: Science China Press

More information

Scope and Contents

Contents

Modern oceans contain large bathymetric highs (spreading oceanic ridges, aseismic ridges or oceanic plateaus and inactive arc ridges) that, in total, constitute more than 20–30% of the total area of the world’s ocean floor. These bathymetric highs may be subducted, and such processes are commonly referred to as ridge subduction. Such ridge subducti...

Alternative Titles

Full title

Ridge subduction, magmatism, and metallogenesis

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2440408871

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2440408871

Other Identifiers

ISSN

1674-7313

E-ISSN

1869-1897

DOI

10.1007/s11430-019-9619-9

How to access this item