Roberts rift, Canyonlands, Utah, a natural hydraulic fracture caused by comet or asteroid impact

Ground Water
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Abstract

The impact that created Upheaval crater in Canyonlands National Park, Utah, is invoked here as the source for energy that simultaneously caused Roberts rift. However, no temporal linkage has been proven between the impact and rifting events.

Roberts rift lies between 22 and 32 km northeast of the Upheaval impact crater on a subradial trend. The fissure contains clasts that were carried as much as 1,000 m upward from Paleozoic sources into the Mesozoic section.

A plausible model for both the rifting and clast movement involves incremental loading of overpressured fluid compartments in the Pennsylvanian Paradox section and attendant hydraulic fracturing of the overlying confining strata during the impact event. The clasts were proppants entrained in upward moving fluids that originated from overpressured aquifers in the Pennsylvanian section or materials eroded from the fissure walls.

Alteration halos and mineralization along the fissure reveal that there was upward leakage of reducing fluids from the overpressured zones following opening of the fissure. The fissure infillings became cemented with time, thus reducing fissure permeabilities to negligible.

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Publication type Article
Publication Subtype Journal Article
Title Roberts rift, Canyonlands, Utah, a natural hydraulic fracture caused by comet or asteroid impact
Series title Ground Water
DOI 10.1111/j.1745-6584.1995.tb00311.x
Volume 33
Issue 4
Year Published 1995
Language English
Publisher National Groundwater Association
Description 9 p.
First page 561
Last page 569
Country United States
State Utah
Other Geospatial Canyonlands National Park, Roberts rift
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