Local subsidence of the Goose Creek oil field

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dc.acquisition-srcReview of GBNEP-6 reference listen_US
dc.call-noAcc# 3366 - Box#11en_US
dc.call-noILL from TAMU-College Stationen_US
dc.contract-noen_US
dc.contributor.authorPratt, W.E.en_US
dc.contributor.authorJohnson, D.W.en_US
dc.contributor.otherThe Journal of Geologyen_US
dc.date.accessioned2010-02-15T17:02:05Z
dc.date.available2010-02-15T17:02:05Z
dc.date.issued1926en_US
dc.degreeen_US
dc.descriptionpgs. 577-590en_US
dc.description-otheren_US
dc.description.abstractIn 1918, Gailard peninsula, the center of the Goose Creek Oil Field, on Galveston Bay, began to subside. The geology of the field and the nature of the subsidence are discussed. It is concluded that subsidence was caused by the extraction of oil, water, gas, and sand from beneath the surface.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.geo-codeGoose Creeken_US
dc.geo-codeGalveston Bayen_US
dc.geo-codeTexas coasten_US
dc.history3/3/05 easen_US
dc.identifier.urihttp://hdl.handle.net/1969.3/21187
dc.latitudeen_US
dc.locationGBIC Archives Collectionen_US
dc.longitudeen_US
dc.notesen_US
dc.placeChicago, ILen_US
dc.publisherThe University of Chicago Pressen_US
dc.relation.ispartofseries3366.00en_US
dc.relation.urien_US
dc.scaleen_US
dc.seriesen_US
dc.subjectsubsidenceen_US
dc.subjectland lossen_US
dc.subjectestuariesen_US
dc.subjectoilen_US
dc.subjectgeologyen_US
dc.subjectpetroleum engineeringen_US
dc.subjectoil and gas fieldsen_US
dc.subjectpetroleumen_US
dc.titleLocal subsidence of the Goose Creek oil fielden_US
dc.typeArticleen_US
dc.universityen_US
dc.vol-issuev.34, no.7en_US

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