| Tecomazuchil Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Geological Formation | 
| Underlies | Chimeco Limestone | 
| Overlies | Acatlán Complex | 
| Lithology | |
| Primary | Silty Sandstone [1] | 
| Location | |
| Region | Puebla Province | 
| Country | Mexico | 
| Type section | |
| Named by | 
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The Tecomazuchil Formation is a geologic formation in Oaxaca, Mexico. It is made up of "a basal conglomerate 135 m thick and predominantly composed of quartz and metamorphic rock fragments, overlain by about 600 m of interbedded tan to red conglomerates, sandstones, and siltstones. The Tecomazuchil Formation overlies unconformably the Acatlán Complex and has been assigned a Middle Jurassic age, though it could represent at least part of the Oxfordian." [2] Fossil Bennettitales have been found in the formation. [3]