A study of sediments from the Juan de Fuca Ridge, Northeast Pacific ocean: with special reference to hydrothermal and diagenetic components
A regional survey of the sedimentology, geochemistry and mineralogy of the Pleistocene and Holocene deep-sea sediments from the Juan de Fuca Ridge between 47°00' and 48°15' North latitude and the adjacent Cascadia Plain indicates a mainly terrigenous, turbiditic source for most sediments i...
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/22550 |