Provenance of the detrital component of deep-sea sediments from the SW Pacific Ocean based on mineralogy, geochemistry and Sr isotopic composition

Clay mineralogy and chemical and strontium isotope compositions have been used to determine the detrital components of deep-sea sediments from the SW Pacific Ocean. Continental detritus derived mainly from the New Zealand landmass is characterised by high illite and chlorite contents, and 87Sr/ 86Sr...

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Veröffentlicht in:	Marine geology 1997-07, Vol.140 (1), p.75-96
Hauptverfasser:	Graham, I.J., Glasby, G.P., Churchman, G.J.
Format:	Artikel
Sprache:	eng
Schlagworte:	deep sea sediments geochemistry Marine mineralogy provenance Sr isotopes SW Pacific
Online-Zugang:	Volltext
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