| Mazatzal Group | |
| Type: | Group |
| Period: | Statherian |
| Prilithology: | Quartzite |
| Otherlithology: | Metaconglomerate |
| Namedfor: | Mazatzal Mountains |
| Namedby: | E.D. Wilson |
| Year Ts: | 1922 |
| Region: | Central Arizona |
| Country: | United States |
| Coordinates: | 33.684°N -111.325°W |
| Unitof: | Tonto Basin Supergroup |
| Underlies: | Hopi Springs Shale |
| Overlies: | Red Rock Rhyolite |
| Thickness: | 2000m (7,000feet) |
The Mazatzal Group is a group of geologic formations that crops out in portions of central Arizona, US. Detrital zircon geochronology establishes a maximum age for the formation of 1660 to 1630 million years (Mya), in the Statherian period of the Precambrian.[1] The group gives its name to the Mazatzal orogeny, a mountain-building event that took place between 1695 and 1630 Mya.
The Mazatzal Group consists mostly of fine-grained light-brown to gray quartzite which often shows cross-bedding; metaconglomerate containing clasts up to 6order=flipNaNorder=flip or more in size; and occasional lenses, up to 150order=flipNaNorder=flip in thickness, of maroon to gray argillite showing ripple marks and mudcracks.[2] The lower beds of the group are intruded by rhyolite domes and sills. The total thickness of the group is up to 2000m (7,000feet).[3] The group lies disconformably on top of the Red Rock Rhyolite[3] and is in turn overlain by the Hopi Springs Shale.
The group crops out in the Mazatzal Mountains,[2] where it has been strongly deformed (with up to 50% shortening to the northwest) and in the Prescott area, where it has been only mildly metamorphosed.[4] It is also present in the upper Salt River canyon. The group gives its name to the Mazatzal orogeny, a mountain-building event that took place between 1695 and 1630 Mya.[3]
In the northern Mazatzal Mountains, the Mazatzal Group is divided (in ascending stratigraphic order) into the Deadman Quartzite, the Maverick Shale, and the Mazatzal Peak Quartzite. In the upper Salt River Canyon, the Mazatzal Group is represented by the White Ledges Formation.[5]
In the Four Peaks area, the Mazatzal Group is divided (in ascending stratigraphic order) into an informal lower quartzite, an informal lower pelite, and the Four Peaks Quartzite. These are interpreted as a single sequence of sediment deposition. The lower quartzite is an extremely pure quartzite up to 60m (200feet) thick. The lower pelite is about 450m (1,480feet) thick and consists of pelite and psammite beds. The Four Peaks Quartzite is up to 400m (1,300feet) thick and is mostly extremely pure quartzite with a few pelite layers.[6]
The unit was first described by E.D. Wilson in 1922 as the Mazatzal Quartzite.[2] It was raised to group rank in 1981 by P. Anderson and W.R. Wirth.[7] The group was assigned to the Tonto Basin Supergroup in 1988 by Karl Karlstrom and Samuel Bowring.[3]