@article{ac9efbbcfbd04efaa270d0366a9eda68,
title = "POLYGONAL CRACKS ON BOUNDING SURFACES IN THE PERMIAN COCONINO SANDSTONE, ARIZONA",
author = "Brand, {Leonard R.}",
note = "The Permian Coconino Sandstone in northern Arizona is a cross-bedded fine sandstone, and most workers consider it to be an eolian deposit, from an extensive desert. Polygonal cracks are common on bounding surfaces in the Coconino Sandstone. Superficially they look like desiccation cracks, but their detailed features are incompatible with that interpretation.",
year = "2018",
doi = "10.1130/abs/2018am-318111",
language = "American English",
volume = "50",
journal = "Geological Society of America Abstracts with Programs",
}