Tres Piedras Orthogneiss
The Tres Piedras Orthogneiss is a pluton in northern New Mexico. It has a U-Pb radiometric age of 1693 Mya, placing it in the Statherian period.[1]
| Tres Piedras Orthogneiss Stratigraphic range: Statherian | |
|---|---|
 Knolls underlain by Tres Piedras Orthogneiss, Tres Piedras, New Mexico, USA | |
| Type | Pluton |
| Lithology | |
| Primary | Orthogneiss |
| Location | |
| Coordinates | 36.649°N 105.990°W |
| Region | Tusas Mountains, New Mexico |
| Country | United States |
| Type section | |
| Named for | Tres Piedras, New Mexico |
| Named by | F. Barker |
| Year defined | 1958 |
  Tres Piedras Orthogneiss (the United States)  Tres Piedras Orthogneiss (New Mexico) | |
Description
Though described as the Tres Piedras Granite in the earlier studies, the unit is more properly described as an orthogneiss.[2] The orthogneiss is pink to reddish-orange and shows faint to obvious foliation. Grain sizes are from 0.5 to 5 mm. Many of the quartz grains are fractured. With a modal composion of 42% quartz, 40% microcline, and 12% albite, it has the composition of a true granite. It has no contact metamorphism with the Moppin Complex, suggesting the country rock was only slightly cooler when the granite was injected.[3]
The orthogneiss crops out around the town of Tres Piedras, New Mexico and intrudes the Moppin Complex to the west in the Tusas Mountains. It may correlate with the San Miguel gneiss in the Nacimiento Mountains.
The pluton is interpreted as possibly a magma chamber associated with Vadito Group volcanism[4] or a stitching pluton associated with the Yavapai-Mazatzal orogenies.[5]
History of investigation
The unit was originally included in the Tusas Granite by Just in his 1937 survey of pegmatites in northern New Mexico.[6] but was designated as the Tres Piedras Granite by Barker in 1958. Barker included exposures near the town of Tres Piedras, along the Rio Tusas, and near Burned Mountain and Hopewell.[7] Wobus and Hedge removed the western outcrops from the pluton[8] based on an unreliable radiometric date[9], but Davis et al. concluded that the Tusas Mountain orthgneiss is likely part of the Tres Piedras Orthogneiss.[10]
Footnotes
- Davis et al. 2011, p.180
- Davis et al. 2011, p.181
- Barker 1958, pp.59-61
- Barker 1958, p.61
- Davis et al. 2011, p.187
- Just 1937, pp.44-45
- Barker 1958, p.59
- Wobus and Hedge 1982
- Davis et al. 2011, p.59
- Davis et al. 2011, p.185
References
- Barker, Fred (1958). "Precambrian and Tertiary geology of Las Tablas quadrangle, New Mexico" (PDF). New Mexico Bureau of Mines and Mineral Resources Bulletin. 45.
- Davis, Peter; Williams, Mike; Karlstrom, Karl (2011). "Structural evolution and timing of deformation along the Proterozoic Spring Creek shear zone of the northern Tusas Mountains, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 62: 177–190.
- Just, Evan (1937). "Geology and Economic Features of the Pegmatites of Taos and Rio Arriba Counties, New Mexico" (PDF). New Mexico School of Mines Bulletin (13).
- Wobus, Reinhard A.; Hedge, Carl E. (October 1982). "Redefinition of the Precambrian Tusas Mountain and Tres Piedras Granites, North-Central New Mexico". The Mountain Geologist. 19 (4): 105–114. Retrieved 9 May 2020.