Farmington Gabbro
Located in the Charlotte Belt of North Carolina is the Farmington Gabbro, located in the Mocksville Complex.[1] The Mocksville Complex consist of metamorphosed/unmetamorphosed gabbros, pyroxenites, hornblendites, wehrlites, granites, and diorites.[2] The plutons in this region formed during the Taconic, Acadian, and Alleghanian orogeny starting on the eastern side of Laurentia.[3] These plutons date back to around 400 Ma, consisting of ultramafic, mafic, and felsic rocks but the Farmington Gabbro is the only pluton on the northwest side of the complex that is unmetamorphosed.[2][4]
| Farmington Gabbro | |
|---|---|
| Stratigraphic range: ~ 400 Ma | |
| Location | |
| Location | Mecklenburg County |
Mocksville Complex[edit]
The Mocksville Complex is surrounded by late Proterozoic granitic, metavolcanic, and gneissic that trends NE-SW over about a 500 km2 area.[2] The complex contains evidence of felsic, mafic, and ultramafic rock types that have been metamorphosed (except farmington gabbro).[2] The age of the complex dates to around 550 million years ago to 650 million years ago. Amphibolites are found in the mafic rocks in the northern section of the complex with bands of plagioclase, quartz, and amphibole with very coarse grained plagioclase and more fine grained amphiboles.[2] Dikes of ultramafic rocks in the complex are peridotites, pyroxenites, and hornblenditites.[2] In the lower end of the complex there are some metamorphosed sedimentary rocks found which are a blend of sandstone and limestone.[2]
For the metagabbros temperatures were found to have reached 550 °C - 650 °C. This was seen by thermal overprint due to Fe-Mg reallocation of existing olivine and calcium rich clinopyroxene.[2] While spinal is found in the complex, garnet is not which infers that the pressure of about 12 kbar or below.[2]
Olivine: medium to high forresteritic (showing a calc-alkali arc environment)
Plagioclase: high in anorthite (showing a calc-alkali arc environment)
Clinopyroxene: high TiO2 and Na2O (showing a calc-alkali arc environment)
Pyroxene: high ratio of tetrahedral Al to titian (showing a calc-alkali arc environment)
Spinal: low Mg, variable Fe3+/ (Fe3++Cr+Al) , and high Cr/(Cr+Al) (showing a calc-alkali arc environment)
Petrology/Mineralogy[edit]
The Farmington Gabbro is postmetamorphic medium to coarse grained plutonic rock next to metagabbros.[2] The unit is surrounded by Proterozoic to early Paleozoic metamorphosed rock.[1] The major and trace elements of the pluton matches the composition of calc-alkaline basaltic magma.[2] The minerals present are plagioclase, hornblende, pyroxenes, olivine, biotite with small amounts of apatite, magnetite, ilmenite, hematite, pyrite, pyrrhotite, and hercynitic spinel.[4][2] The main texture in the gabbro is ophitic to sub-ophitic, but hornblende and plagioclase are subhedral to anhedral grains.[2] Plagioclase is twinned with little zoning.[2] The pyroxene content is mostly clinopyroxene with some orthopyroxene.[2]
Mineral differences[edit]
The Famrinto Gabbro has two gabbronorites that are slightly different in mineralogy and texture.[1] One rock type is a olivine, pyroxene, hornblende while the other has clinopyroxene, olivine, and plagioclase gabbronorite with cumulus texture.[1] The hornblende gabbronorite is a dark grey to grey-green with a fine to medium grained texture.[5]
| Elements shown in wt% | |||
| Sample | 1 | 2 | 3 |
| SiO2 | 48.22 | 47.93 | 45.56 |
| TiO2 | 0.60 | 0.62 | 0.19 |
| Al2O3 | 19.35 | 18.20 | 14.95 |
| MnO | 0.15 | 0.15 | 0.11 |
| MgO | 8.97 | 8.73 | 16.66 |
| FeO | 7.82 | 6.22 | 5.32 |
| CaO | 10.18 | 12.71 | 15.64 |
| Na2O | 3.88 | 3.28 | 0.58 |
| K2O | 0.14 | 0.13 | 0.33 |
| P2O5 | 0.02 | 0.05 | 0.01 |
| Total | 99.34 | 98.02 | 99.34 |
Outcrops[edit]
The area of gabbro-diorite intrusions stretches about 720 km long.[6] They are seen as large boulders and on the side of highway 40 NC and highway 158 NC where the hill was cut for the road way.[1] The Mocksville complex consist mostly of metagabbro, but there are outcrops where you can see the contact between the metagabbro rocks and the gabbro (Farmington).[1] The contact could be easily seen because the Farmington Gabbro is the only non-metamorphosed rock unit in this area of plutons so distinguishing between a metagabbro and gabbro may be unchallenging due to the difference in foliation and lineation.[2]
The Vulcan Smith Materials Company mines Farmington Gabbro as an aggregate located off of Highway 40 NC.
References[edit]
- ^ a b c d e f g Esawi, E. K. (2004-04-01). "Evidence from the Farmington pluton for early Devonian subduction-related magmatism in the Carolina zone of central North Carolina". Journal of Geodynamics. Tectonics of the Appalachian Belt. 37 (3): 531–548. Bibcode:2004JGeo...37..531E. doi:10.1016/j.jog.2004.02.019. ISSN 0264-3707.
- ^ a b c d e f g h i j k l m n o p Esawi, E. K. (January 2012). "The mafic and ultramafic rocks of the Mocksville complex of Central North Carolina: Petrogenetic and tectonic implications". Mineralogy and Petrology. 104 (1–2): 15–27. Bibcode:2012MinPe.104...15E. doi:10.1007/s00710-011-0180-8. ISSN 0930-0708. S2CID 140740572.
- ^ Secor, Donald T.; Snoke, Arthur W.; Dallmeyer, R. David (1986-11-01). "Character of the Alleghanian orogeny in the southern Appalachians: Part III. Regional tectonic relations". GSA Bulletin. 97 (11): 1345–1353. doi:10.1130/0016-7606(1986)97<1345:COTAOI>2.0.CO;2. ISSN 0016-7606.
- ^ a b McSween, H. Y.; Sando, T. W.; Clark, S. R.; Harden, J. T.; Strange, E. A. (1984-05-01). "The gabbro-metagabbro association of the Southern Appalachian Piedmont". American Journal of Science. 284 (4–5): 437–461. Bibcode:1984AmJS..284..437M. doi:10.2475/ajs.284.4-5.437. ISSN 0002-9599.[permanent dead link]
- ^ Wilson, Frederick A. (1983). "Geophysical and geologic studies in southern Mecklenburg County and vicinity, North Carolina and South Carolina". Open-File Report. doi:10.3133/ofr8393.
- ^ Butler, J. Robert; Ragland, Paul C. (1969-10-01). "A petrochemical survey of plutonic intrusions in the Piedmont, Southeastern Appalachians, U.S.A." Contributions to Mineralogy and Petrology. 24 (2): 164–190. Bibcode:1969CoMP...24..164B. doi:10.1007/BF00376889. ISSN 1432-0967. S2CID 129688594.