The Sandia granite is a pluton in central New Mexico. It has a radiometric age of 1453±12 Ma, corresponding to the Calymmian period.
| Sandia granite | |
|---|---|
| Stratigraphic range: | |
 Outcrops of Sandia granite, Tijeras Canyon, New Mexico, USA | |
| Type | Pluton |
| Lithology | |
| Primary | Monzogranite |
| Other | Granodiorite |
| Location | |
| Coordinates | 35°07′01″N 106°26′20″W / 35.117°N 106.439°W |
| Region | New Mexico |
| Country | United States |
| Type section | |
| Named for | Sandia Mountains |
| Named by | Kelley and Northrop |
| Year defined | 1975 |
  Sandia granite (the United States)  Sandia granite (New Mexico) | |
Description
edit
The Sandia granite is prominently exposed along the east flank of the Rio Grande rift, with almost 1.5 kilometres (4,900 feet) of exposure at Sandia Crest. It extends from Placitas to Tijeras Canyon. Its radiometric age is 1453±12 Ma.[1]
The pluton is a single body with significant heterogeneities. The primary phase is monzogranite with a secondary phase of granodiorite. It is notable for the presence of local outcrops of orbicular granite. Both major phases contain diorite inclusions that are interpreted as co-mingled melts. Exposures are typically gray to pink, medium-to-coarse grained, monzogranite. Aplite and pegmatite dikes crosscut by quartz veins are common. The average modal composition is 28% quartz, 25% potassium feldspar, 38% plagioclase, 8% biotite, and 1% accessory minerals, including magnetite, titanite, zircon, hornblende, apatite, and muscovite.[1]
There are three generations of deformation preserved in the contact aureole that indicate regional deformation. Microstructure and foliation in the aureole indicate east-west compression and north-south extension during and shortly after pluton emplacement, but the pluton interior is undeformed. Pluton emplacement involving heating to ~650°C at pressures of 2-3 kbars, corresponding to a depth of 7-10 km.[1]
The pluton is interpreted as having been emplaced syntectonically at middle crustal depth during the Picuris orogeny. Though there is no local extrusive equivalent, the western Granite-Rhyolite provinces east of the Rocky Mountains may be an extrusive equivalent.[2]
History of investigation
editThe unit was first defined by Kelley and Northrop in 1975.[3] The name has continued in common use[1] in spite of being preempted by the Sandia Formation.[4]
Footnotes
edit- ^ a b c d Grambling et al. 2016, pp. 172–173.
- ^ Grambling et al. 2016.
- ^ Kelley & Northrop 1975.
- ^ GEOLEX 2020.
References
edit- "Sandia". GEOLEX. August 2020. Retrieved 28 February 2021.
- Grambling, Tyler A.; Karlstrom, Karl E.; Holland, Mark E.; Grambling, Nadine L. (2016). "Proterozoic magmatism and regional contact metamorphism in the Sandia-Manzano Mountains, New Mexico, USA" (PDF). New Mexico Geological Society Field Conference Series. 67: 169–175. Retrieved 27 May 2020.
- Kelley, V.C.; Northrop, S.A. (1975). "Geology of the Sandia Mountains and vicinity, New Mexico" (PDF). New Mexico Bureau of Mines and Mineral Resources Memoir. 29. Retrieved 21 September 2020.