Thesis (Ph. D.)--University of Texas at Austin, 2002. / Includes bibliographical references. Available also in an electronic version.

Thesis (M.S.)--Oregon State University, 2007. / Printout. Includes bibliographical references (leaves 67-71). Also available on the World Wide Web.

Thesis (Ph. D.)--University of Chicago, 1922. / "A Dissertation, submitted to the Faculty of the Ogden Graduate School of Science in candidacy for the Degree of Doctor of Philosophy, Department of Geology." "Private edition, distributed by the University of Chicago Libraries, Chicago, Illinois." "Reprinted from U.S. Geological survey, Professional paper 128 ... 1920." Includes bibliographical references.

xi, 60 p. : ill. (some col.), maps (some col.). A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number. / I present an alternative approach to determine the magnitude and direction of extension in the Basin and Range Province at the north end of Summer Lake basin using GIS techniques. Offset across 161 faults and tilting of 56 fault blocks were estimated to calculate extension as a function of azimuth in this area. The orientation of a representative set of slickenlines was collected in the field to assign average values for the GIS analysis. Azimuthal variation of extension is consistent with a strain ellipse indicating plane strain with extension of 1.5 to 5.5 percent along the maximum extension direction of N75E and no extension along the minimum N15W axis. Blocks tilt on average 60° from the maximum extension direction, suggesting the underlying detachment dips -N15E. This technique allows strain associated with the numerous small faults to be added to the sparse large faults for a complete regional analysis. / Committee in Charge: Dr. Ray Weldon, Chair; Dr. David Schmidt; Dr. Marli Miller

The Indianhead Creek map-area is located directly north of the Clearwater River and encompasses a four mile length of the third range of the Alberta Rocky Mountains. The map-area contains one minor thrust fault, a portion of the Third Range thrust fault and a series of four large normal faults. The normal fault blocks are tilted to the south with the lower beds of each fault block being progressively truncated by the slightly northward dipping Third Range thrust fault. Two of these normal faults also cut through the Third Range thrust fault and continue into the underlying formations with a large loss in stratigraphic separation. Two hypotheses are proposed to explain the time relationships and causes of normal faulting. The first hypothesis states that the normal faulting and the tilting of the normal fault blocks occurred before the development of the Third Range thrust fault. Then during thrust faulting, the minor thrust and the progressive truncation of the lower beds of each normal fault block occurred. A recurrence of normal faulting took place after the completion of thrust faulting in which the Third Range thrust fault and the underlying formations were displaced. The second period of normal faulting developed along the planes of the previously existing normal faults. The second hypothesis states that the normal faulting, the tilting of the normal fault blocks, and the thrust faulting developed concurrently. A monoclinal fold in the plane of the Third Range thrust fault is proposed in order to explain the progressively southward truncation of the lower beds of the tilted normal fault blocks and the large loss in stratigraphic separation as two of the normal faults pass through the thrust fault. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate

Thesis. 1975. Ph.D.--Massachusetts Institute of Technology. Dept. of Earth and Planetary Sciences. / Bibliography: leaves 422-441. / by Raymon Lee Brown, Jr. / Ph.D.

Recent observations have highlighted the shortcomings of traditional thinking about faults and fault patterns. The slip model of faulting, developed by Ze'ev Reches, suggests that four sets of faults, arranged in orthorhombic symmetry about the principal strain axes, can accommodate general, three-dimensional strain. Classic conjugate faults are simply a special case of plane strain. Careful analysis of orthorhombic fault patterns and the tenets of the slip model has led to the development of a practical method for decoding the strain significance of fault systems developed in three-dimensional strain fields. The methods are implicit in a model here called the odd-axis model. This new model calls special attention to the odd axis: the one principal strain with sign opposite the other two, assuming a constant volume deformation. Odd-axis medel equations relate fault set geometry to principal strain magnitudes or ratios, the internal friction angle, φ, and the ratio of average fault slip to average spacing between faults of the same set, R. For systems where R < 0.1, the three principal strain ratios are given by tan²α, -sin²α, and -COS²α, where α is the strike of the fault set(s) measured in the plane perpendicular to the odd axis. The model also predicts slip vector orientations as functions of principal strain ratios and orientations. The kinematic implications of the odd-axis model are compatible with those of the slip model. In this first quantitative field test, both fault models are applied to the Chimney Rock array, a system of orthorhombic faults in the northern San Rafael Swell of central Utah. The odd-axis model uses fault plane and slip vector data from Chimney Rock to predict principal strain ratios (ε(y)/ε(x), ε(y)/ε(z), and ε(x)/ε(z)) of .20, -.16, and -.84. These compare extremely well with the observed values, based on fault separation measurements, of .17, -.15, and -.85. The value of ε(y)/ε(z) predicted by the slip model, -.16, matches exactly the value predicted by the odd-axis model and nearly matches the observed value, which is -.15. The success of the field test at Chimney Rock, and the conceptual agreement of both models, suggest that the new theory can accurately relate orthorhombic fault geometries and three-dimensional strain fields. Furthermore, the results underscore how important it is for geologists to recognize the sensitivity of fault geometry and kinematics to three-dimensional strain.

Thesis (Ph. D.)--Dept. of Geosciences and School of Computing and Engineering. University of Missouri--Kansas City, 2005. / "A dissertation in geosciences and computer networking." Advisor: Tina M. Niemi. Typescript. Vita. Description based on contents viewed Mar. 12, 2007; title from "catalog record" of the print edition. Includes bibliographical references (leaves 331-341). Online version of the print edition.

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