Browsing Geological Sciences electronic theses and dissertations (MU) by Thesis Advisor "Bauer, Robert L. (Robert Louis)"
Now showing items 1-12 of 12
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2D and 3D modeling of the Laramide fold geometry of Derby Dome and its en echelon interchange with Dallas Dome, southern Wind River Basin, Wyoming
(University of Missouri--Columbia, 2014)The Wind River Mountains of central Wyoming formed as a basement-cored uplift during the Laramide orogeny (ca. ~75-35 Ma) and produced a series of left stepping, en echelon NW-SE trending folds, including Dallas Dome and ... -
Analysis of quaternary faults and associated deformation of sedimentary basin fill : inner continental borderland of southern California
(University of Missouri--Columbia, 2012)The San Andreas fault system is distributed across hundreds of kilometers in southern California. This transform system includes offshore faults along the shelf, slope and across the Gulf of Santa Catalina basin (GSCB) -- ... -
Analysis of the interchange between en echelon basin-margin Laramide folds adjacent to the Wind River Mountains, Wyoming
(University of Missouri--Columbia, 2013)[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT AUTHOR'S REQUEST.] Uplift of the basement-cored Wind River Mountains during the Laramide orogeny (ca. 75- 45 Ma) produced a series of subsidiary en echelon NW-SE trending ... -
Geologic mapping, structural analysis, and paleostress modeling of late-stage N-S laramide shortening in the lander NW quadrangle, Wind River Basin, Wyoming
(University of Missouri--Columbia, 2015)Uplift of the basement-cored Wind River Mountains during the Laramide orogeny (ca. 75-45 Ma) produced a series of en echelon NW-SE trending basin margin folds along the southwestern margin of the Wind River basin. The ... -
Laramide stress conditions and deformation mechanisms during the formation of Derby and Dallas Domes, Weiser Pass Quadrangle, Wind River Mountains, Wyoming
(University of Missouri--Columbia, 2007)Uplift of the Wind River Mountains during the Laramide orogeny (ca. 80-40 Ma) produced a NNW-SSE series of southwest-verging, asymmetric, doubly plunging folds along the northeastern margin of the range. This fold series, ... -
Laramide stress conditions and deformation mechanisms during the formation of Hudson and Dallas Domes, Lander Quadrangle, Wind River Mountains, Lander, Wyoming
(University of Missouri--Columbia, 2008)Laramide fold forms along the northeastern flank of the Wind River Mountains in west central Wyoming include a series of doubly plunging folds arranged in a left-stepping en echelon pattern. The fold patterns and geometries ... -
Late-stage Laramide reactivation of Precambrian structures : evidence for [about]N-S Laramide shortening along the southeastern margin of the Wind River Mountains, Wyoming
(University of Missouri--Columbia, 2012)Deformation along the southeastern margin of the Wind River Mountains during the late stages of the Laramide orogeny is a result of local [about]N-S Laramide shortening, which is in contrast to the regional NE-SW shortening ... -
Late-stage N-S shortening and fold offset during Laramide deformation along the southeastern margin of the Wind River Mountains, Wyoming
(University of Missouri--Columbia, 2011)Uplift of the basement-cored Wind River Mountains during the Laramide orogeny (ca. 75-45 Ma) produced a series of subsidiary NW-SE trending folds along the southwestern margin of the Wind River Basin. These folds are ... -
Mechanisms for the formation of spiraled inclusion trails in garnet porphyroblasts from the Precambrian core of the Laramie Mountains, southeastern Wyoming
(University of Missouri--Columbia, 2013)Relationships between deformation fabrics and porphyroblasts have been used to evaluate the metamorphic and deformational histories of mountain belts. However, some porphyroblast-fabric relationships, such as those of ... -
Structural analysis of basin margin laramide folding and fault reactivation in the south-central Wind River Basin, Schoettlin Mountain quadrangle, Fremont County, Wyoming
(University of Missouri--Columbia, 2010)[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] The southwestern margin of the Wind River basin contains a series of southwest verging, left-stepping, en-echelon Laramide-aged folds that fold Paleozoic ... -
Structural geology and contact metamorphism along the northwestern thermal aureole of the Laramie anorthosite complex, Central Laramie Mountains, Wyoming
(University of Missouri--Columbia, 2013)[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT AUTHOR'S REQUEST.] The southeastern margin of the Archean Wyoming craton has undergone a complex history of Proterozoic deformation and metamorphism. The Archean rocks ... -
Structural geology and tectonics of the paleoproterozoic rocks of the Mount Rushmore Quadangle, Black Hills, Souh Dakota
(University of Missouri--Columbia, 2006)The Paleoproterozoic assembly of Laurentia occurred between ̃1.96 to 1.70 Ga, and continued with the accretion of island arc terranes until about 1.63 Ga. The Black Hills, South Dakota lie along the eastern margin of the ...