Active surface faulting, Texas coastal zone.

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dc.acquisition-srcen_US
dc.call-noen_US
dc.contract-noen_US
dc.contributor.authorKreitler, C.W.en_US
dc.contributor.otherAmerican Association of Petroleum Geologists Bulletin.en_US
dc.date.accessioned2010-02-15T16:48:35Z
dc.date.available2010-02-15T16:48:35Z
dc.date.issued1976en_US
dc.degreeen_US
dc.descriptionp. 689.en_US
dc.description-otheren_US
dc.description.abstractTopographic escarpments coincident with active faults in the Houston area existed before major ground water withdrawals. However, ground water withdrawal is the primary mechanism for fault activation in Harris and Galveston Counties.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.geo-codeHarris Countyen_US
dc.geo-codeHoustonen_US
dc.geo-codeGalveston Countyen_US
dc.historyen_US
dc.identifier.urihttp://hdl.handle.net/1969.3/18912
dc.latitudeen_US
dc.locationTAMUG periodical collectionen_US
dc.longitudeen_US
dc.notesen_US
dc.placeen_US
dc.publisheren_US
dc.relation.ispartofseries1177.00en_US
dc.relation.urien_US
dc.scaleen_US
dc.seriesen_US
dc.subjectgeologyen_US
dc.subjectgeological structuresen_US
dc.subjectfaultsen_US
dc.subjectfaciesen_US
dc.subjectground wateren_US
dc.titleActive surface faulting, Texas coastal zone.en_US
dc.typeArticleen_US
dc.universityen_US
dc.vol-issue60(4)en_US

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