Jointing History of the Palo Duro Basin

dc.creatorCollins, Edward W.
dc.date.accessioned2024-03-11T15:44:53Z
dc.date.available2024-03-11T15:44:53Z
dc.date.issued1984
dc.description.abstractJoints are fractures or partings in a rock that exhibit no displacement (Bates and Jackson, 1980, p. 334). Two styles of joints are systematic joints and nonsystematic joints (Hodgson, 1961). Systematic joints occur in sets. Joints composing each set are subparallel and are commonly orthogonal to the upper and lower surfaces of the rock units in which they are present. Nonsystematic joints display no preferred orientation and truncate against systematic joints.
dc.description.departmentBureau of Economic Geology
dc.identifier.urihttps://hdl.handle.net/2152/124165
dc.identifier.urihttps://doi.org/10.26153/tsw/50777
dc.relation.ispartofContract Reports
dc.rights.restrictionOpen
dc.subjectgeology
dc.subjectPalo Duro Basin
dc.subjectTexas
dc.titleJointing History of the Palo Duro Basin
dc.typeOther

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