Browsing by Subject "Folds (Geology)"
Now showing items 1-11 of 11
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The cow creek anticline: an example of disharmonic folding along the front of the Big Horn Mountains (Texas A&M University, 1983)Not available
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(Texas A&M University. Libraries, 1984)18 mesoscopic kinkbands have been studied in the Jura Mountains and the Chaines Subalpines (Switzerland and France). The kinkbands have formed in well-bedded, micritic limestones (5 to 50 cm bedding thickness) with interbedded ...
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(Texas A&M University, 1978)Not available
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(Texas A&M University. Libraries, 1983)Growth faults and related folds are geologically and economically the most important structural features in the Gulf Coast province. Most existing theories do not adequately explain the observed fold geometries, and ...
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(Texas A&M University. Libraries, 1986)The concept of forced folding (Stearns, 1971,1978) forms the basis for the research reported here on Rattlesnake Mountain Anticline. Field observations address fold formation with respect to: causative basement blocks, the ...
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(Texas A&M University, 1976)Not available
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(Texas A&M University. Libraries, 1990)To better understand the process of initiation and propagation of thrust faults in layered rock and die role of weak bed-parallel surfaces in the deformation, we mapped wedge faults (WFs) and bed-parallel faults and described ...
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(Texas A&M University. Libraries, 1984)Comparisons of field, experimental, and theoretical data on the deformation in a sedimentary layer due to movement on an underlying, pre-existing basement fault, provide the basis for a conceptual normal-fault model in ...
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(Texas A&M University. Libraries, 1976)Previous experimental folding of single beams of Indiana limestone provides stress-strain curves ana evidence of buckling instability. These experimental results provide the general information needed to make incremental ...
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(Texas A&M University. Libraries, 1977)The vertical movements of basement-blocks and the resulting folds in the overlying sedimentary veneer that characterize the deformation style in the Rocky Mountain foreland are amenable to simple two-dimensional kinematic ...