Paleo-fluid migration and diagenesis in the Pennsylvanian-Permian Fountain Formation
<p> The Pennsylvanian-Permian Fountain Formation is an arkosic conglomeratic sandstone that was deposited in fluvial environments along the eastern flanks of the ancestral Rocky Mountains. The formation owes its pinkish red color to hematite cement that was precipitated early in its diagenetic...
| Main Author: | |
|---|---|
| Language: | EN |
| Published: |
Colorado State University
2013
|
| Subjects: | |
| Online Access: | http://pqdtopen.proquest.com/#viewpdf?dispub=1544780 |