A theory relating high temperatures and overpressures.

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dc.acquisition-srcen_US
dc.call-noen_US
dc.contract-noen_US
dc.contributor.authorLewis, C.R.en_US
dc.contributor.authorRose, S.C.en_US
dc.contributor.otherJournal of Petroleum Technologyen_US
dc.date.accessioned2010-02-15T16:48:39Z
dc.date.available2010-02-15T16:48:39Z
dc.date.issued1969en_US
dc.degreeen_US
dc.descriptionp. 11-16.en_US
dc.description-otheren_US
dc.description.abstractThe theory proposed in this paper is that an overpressured zone, because it is less compacted, constitutes a thermal barrier. That is, this uncompacted zone contains excess amounts of water, and water has three times the insulating value of the rock matrix. This theory is discussed and then compared with field data from two areas, N.E. Thompsonville field in South Texas and offshore Texas in the Galveston area. Practical applications of the theory are considered.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.geo-codeGalveston Bayen_US
dc.historyen_US
dc.identifier.urihttp://hdl.handle.net/1969.3/18924
dc.latitudeen_US
dc.locationGBIC Collection file roomen_US
dc.longitudeen_US
dc.notesen_US
dc.placeen_US
dc.publisheren_US
dc.relation.ispartofseries1188.00en_US
dc.relation.urien_US
dc.scaleen_US
dc.seriesen_US
dc.subjectgeologyen_US
dc.subjectsediment temperatureen_US
dc.subjectpressureen_US
dc.subjectstructural geologyen_US
dc.subjecttectonicsen_US
dc.titleA theory relating high temperatures and overpressures.en_US
dc.typeArticleen_US
dc.universityen_US
dc.vol-issue22(1)en_US

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