TRACE METAL GEOCHEMISTRY WITHIN THE OXYGEN MINIMUM ZONE OFF CENTRAL-SOUTH CHILE MARGIN (36°S):THE USE OF Cd, Co, U AND Mo AS PROXIES OF PALEOPRODUCTIVITY IN SEDIMENTS.

dc.contributorUniversidad Católica del Norte
dc.date.accessioned2016-12-20T13:32:47Z
dc.date.accessioned2018-06-13T23:00:33Z
dc.date.available2016-12-20T13:32:47Z
dc.date.available2018-06-13T23:00:33Z
dc.date.created2016-12-20T13:32:47Z
dc.date.issued2006
dc.identifierhttp://hdl.handle.net/10533/164014
dc.identifier1061214
dc.identifierF
dc.identifier9522477
dc.identifier6
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1542836
dc.relationhandle/10533/111547
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1061214
dc.relationhandle/10533/111541
dc.relationhandle/10533/108045
dc.relationinstname: Conicyt
dc.relationreponame: Repositorio Digital RI2.0
dc.rightsinfo:eu-repo/semantics/openAcces
dc.titleTRACE METAL GEOCHEMISTRY WITHIN THE OXYGEN MINIMUM ZONE OFF CENTRAL-SOUTH CHILE MARGIN (36°S):THE USE OF Cd, Co, U AND Mo AS PROXIES OF PALEOPRODUCTIVITY IN SEDIMENTS.
dc.typeProyecto


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