Areas of ground subsidence due to geofluid withdrawal.

dc.acquisition-srcen_US
dc.call-noen_US
dc.contract-noen_US
dc.contributor.authorGrimsrud, G.P.en_US
dc.contributor.authorTurner, B.L.en_US
dc.contributor.authorFrame, P.A.en_US
dc.contributor.otheren_US
dc.date.accessioned2010-02-15T16:52:26Z
dc.date.available2010-02-15T16:52:26Z
dc.date.issued1978en_US
dc.degreeen_US
dc.description330 p.en_US
dc.description-otheren_US
dc.description.abstractDetailed information is provided on four geothermal areas with histories of subsidence. These were selected on the basis of: physical relevance of subsidence areas to high priorty US geothermal sites in terms of withdrawn geofluid type, reservoir depth, reservoir geology and rock characteristics, and overburden characteristics; and data completeness, quality, and availability. The four areas are: Chocolate Bayou, Raft River Valley, Wairakei, and the Geysers.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.geo-codeChocolate Bayouen_US
dc.historyen_US
dc.identifier.urihttp://hdl.handle.net/1969.3/19548
dc.latitudeen_US
dc.locationNOT AVAILABLE IN-HOUSE.en_US
dc.longitudeen_US
dc.notesen_US
dc.placeBerkeley, California:en_US
dc.publisherUniversity of California at Berkeley. Lawrence Berkeley Lab., Department of Energy.en_US
dc.relation.ispartofseries1793.00en_US
dc.relation.urien_US
dc.scaleen_US
dc.seriesen_US
dc.subjectsubsidenceen_US
dc.subjectground wateren_US
dc.subjectreservoirsen_US
dc.subjectgeothermal energyen_US
dc.subjectgeologyen_US
dc.titleAreas of ground subsidence due to geofluid withdrawal.en_US
dc.typeBooken_US
dc.universityen_US
dc.vol-issueen_US

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