New rock formation discovered in Colorado
- Date:
- September 23, 2014
- Source:
- Geological Society of America
- Summary:
- An astonishing new rock formation has been revealed in the Colorado Rockies, and it exists in a deeply perplexing relationship with older rocks. Named the Tava sandstone, this sedimentary rock forms intrusions within the ancient granites and gneisses that form the backbone of the Front Range. The relationship is fascinating because it is backward: ordinarily, it is igneous rocks such as granite that would that intrude into sedimentary rocks.
- Share:
An astonishing new rock formation has been revealed in the Colorado Rockies, and it exists in a deeply perplexing relationship with older rocks. Named the Tava sandstone, this sedimentary rock forms intrusions within the ancient granites and gneisses that form the backbone of the Front Range. The relationship is fascinating because it is backward: ordinarily, it is igneous rocks such as granite that would that intrude into sedimentary rocks.
According to authors Christine Smith Siddoway and George E. Gehrels, to find sandstone injected into granite is utterly uncommon -- the extensive system that is found in Colorado may be unique in the world. There is evidence that the process of formation involved very large earthquakes, or possibly another type of catastrophic event, causing liquefaction of sediment, what they call "'natural fracking' in a certain sense!"
Equally astonishing is the time of formation of the Tava sandstone, determined from detrital zircon analysis: the Tava proves to be from a time period ~750 million years ago, which was not known to be represented in the Colorado Rockies: the Cryogenian Period.
Story Source:
Materials provided by Geological Society of America. Note: Content may be edited for style and length.
Journal Reference:
- C. S. Siddoway, G. E. Gehrels. Basement-hosted sandstone injectites of Colorado: A vestige of the Neoproterozoic revealed through detrital zircon provenance analysis. Lithosphere, 2014; DOI: 10.1130/L390.1
Cite This Page: