Late Cretaceous to Quaternary sedimentary development of the Lord Howe Rise and the Dampier Ridge

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dc.contributor.authorCovey, Wilkes Perry.
dc.contributor.departmentOceanography
dc.date.accessioned2021-09-13T19:31:54Z
dc.date.available2021-09-13T19:31:54Z
dc.date.issued1973
dc.description.abstractApproximately 3,500 km of continuous seismic reflection profiles and the stratigraphy at Deep Sea Drilling Project (DSDP) Sites 207 and 208 from Leg 21 have been used to interpret the Late Cretaceous to Quaternary sedimentary development of the Lord Howe
dc.description.degreeM.S.
dc.identifier.urihttp://hdl.handle.net/10125/76165
dc.languageeng
dc.publisherUniversity of Hawaii at Manoa
dc.relationTheses for the degree of Master of Science (University of Hawaii at Manoa). Oceanography
dc.subjectSubmarine geology
dc.subject.lcshMarine sediments--Tasman Sea.
dc.subject.lcshSubmarine geology.
dc.titleLate Cretaceous to Quaternary sedimentary development of the Lord Howe Rise and the Dampier Ridge
dc.title.alternativeLord Howe Rise and the Dampier Ridge
dc.typeThesis
dc.type.dcmiText
local.identifier.callnumberQ111 .H3 no.1175
local.identifier.voyagerid513137

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