Petrogenesis of basaltic rocks from the Mariana Trough

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dc.contributor.authorFryer, Patricia
dc.contributor.departmentGeology and Geophysics
dc.date.accessioned2021-09-13T19:30:12Z
dc.date.available2021-09-13T19:30:12Z
dc.date.issued1981
dc.description.abstractThe Mariana Trough, a young, actively spreading back-arc bas in, 1s very similar tectonically to normal mid-ocean ridges. The major difference 1s proximity of the spreading center 1n the Mariana Trough to an active subduction zone. Basaltic glasses retrie
dc.description.degreePh.D.
dc.identifier.urihttp://hdl.handle.net/10125/76137
dc.languageeng
dc.publisherUniversity of Hawaii at Manoa
dc.relationTheses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Geology and Geophysics
dc.subjectBasalt
dc.subject.lcshPetrology--Mariana Islands.
dc.subject.lcshIsland arcs--Mariana Islands.
dc.subject.lcshBasalt--Mariana Islands.
dc.titlePetrogenesis of basaltic rocks from the Mariana Trough
dc.typeThesis
dc.type.dcmiText
dcterms.spatialNorth Pacific Ocean--Mariana Trench
local.identifier.callnumberAC1 .H3 no.1474
local.identifier.voyagerid1151439

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