Oblique slip in Laramide foreland arches
Conference
·
· Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5878948
- Colorado State Univ., Fort Collins, CO (United States). Dept. of Earth Resources
Don Wise was one of the first structural geologists to recognize the complex, four-dimensional (space and time) nature of basement-involved faulting in the Rocky Mountain foreland. His focus on both small scale kinematic indicators and regional tectonic hypotheses has provided a launching point for many Rocky Mountain geologists. The implications of the anastomosing patterns of Laramide foreland arches on models of regional stress and strain have provoked considerable debate. Hypotheses range from those invoking multiple stages of lateral compression from different directions to single-stage models necessitating a component of strike-slip motion in east-west and north-south arches. These hypotheses were tested using slickenline analysis of minor faulting in structures with different orientations. In Wyoming, structures paralleling the dominant northwest structural trend have slickenlines in the NE-SW vertical plane, consistent with shortening and compression in this direction. The east-west Owl Creek and Casper Mountain structures also have NE-SW trending slickenlines, indicating slip oblique to these arches. In Colorado, minor faults in the north-south margin of the northeastern Front Range also indicate oblique slip, with shortening in the NE-SW quadrant. The actual trend of the slickenlines is more easterly, however, suggesting a change of slip trajectory with latitude, not time, possibly in response to identation by the Colorado Plateau.
- OSTI ID:
- 5878948
- Report Number(s):
- CONF-9303211--
- Conference Information:
- Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 25:2
- Country of Publication:
- United States
- Language:
- English
Similar Records
Oblique convergence during northeast-southwest Laramide compression along the east-west Owl Creek and Casper Mountain arches, central Wyoming
Oil and gas prospecting beneath Precambrian of Foreland thrust plates in Rocky Mountains
Structural relationships of northern and central parts of Emigrant Gap anticline, Natrona County, Wyoming
Journal Article
·
Fri Sep 01 00:00:00 EDT 1995
· AAPG Bulletin
·
OSTI ID:159909
Oil and gas prospecting beneath Precambrian of Foreland thrust plates in Rocky Mountains
Journal Article
·
Fri Dec 31 23:00:00 EST 1982
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:5718030
Structural relationships of northern and central parts of Emigrant Gap anticline, Natrona County, Wyoming
Conference
·
Fri Aug 01 00:00:00 EDT 1986
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:7230263