The formation is cut by thrust and strike-slip faults consistent with east-northeast to east-trending tectonic compression of the late stages of the Laramide Orogeny.[1]
The beds now designated as the Diamond Tail Formation were originally part of F.V. Hayden'sGalisteo sand group.[3] By 1997, it was clear that these beds were separated from the remainder of the Galisteo by a significant regional unconformity, and they were split off into the Diamond Tail Formation, named after exposures near Diamond Tail Ranch.[2]
Erslev, Eric A. (1 January 2001). "Multistage, multidirectional Tertiary shortening and compression in north-central New Mexico". GSA Bulletin. 113 (1): 63–74. doi:10.1130/0016-7606(2001)113<0063:MMTSAC>2.0.CO;2.
Hayden, F.V. (1869). United States Geologic Survey of New Mexico and Colorado.