Browsing by Subject "Thrust faults (Geology)"
Now showing items 1-5 of 5
-
(Texas A&M University, 1982)Not available
-
(Texas A&M University. Libraries, 1992)Map-view curves in thrust-fault traces are common in fold-and-thrust belts. Frontal-transverse-frontal ramp geometries are typically the reason. However, not all curves in thrust-fault traces can be related directly to ...
-
(Texas A&M University. Libraries, 1990)The South Fork thrust, a hanging wall imbricate of the Absaroka thrust sheet, southwest Wyoming, has a high angle (~70°), small displacement (~900 ft.), oblique ramp in the hanging wall and footwall. Two penetrative ...
-
(Texas A&M University. Libraries, 1990)Fabrics in fault rocks along the Lewis thrust fault at Marias Pass, northwest Montana, depend on lithology. Fault rocks derived from hanging-wall dolomite are random-fabric cataclasites, whereas fault rocks that include ...
-
(Texas A&M University. Libraries, 1989)Boudin wavelength to thickness ratios are determined by: (1) the value of the power-law exponent in the layer, (2) the ratio of layer strength to confining medium strength; and (3) the ease of slip on the layer-medium ...