Minerals/Carbonides
Carbonides are naturally occurring minerals composed of 50 atomic percent, or more, carbon. Carbonide-like minerals with greater than 25 at % carbon are also included. This separates carbon containing minerals from carbonates which are at most 25 at % carbon.

Diamonds Edit
Def. "[a] naturally occurring, glimmering glass-like allotrope of carbon in which each atom is surrounded by four others in the form of a tetrahedron"[1] is called a diamond.
The diamond imaged on the right has been estimated to be just over 1.5 carats. It measures 5 mm on edge. Although it might seem small, it has wonderful visual impact because of the clarity and perch on matrix. Embedded perhaps 50% in the matrix, so you know it is real. What is more, you can look right through the diamond to the matrix underneath! Around the diamond is a thin white layer you sometimes see, which indicates not glue but rather an alteration in the surrounding rock due to the chemical heat of formation of the crystal and is a good indication of its origins as natural.
Graphites Edit
Graphite is a hexagonal form of carbon that often appears as tabular crystals.
Chaoites Edit
Chaoites are another hexagonal form of native carbon. It occurs as "thin lamellae (3-15 microns wide), alternating with graphite and perpendicular to the {0001} face of graphite."[2]
"Occurs in association with graphite, zircon, and rutile in shocked graphite gneisses from Mottingen in the Ries Crater, Germany. Also observed from the Goalpara and Dyalpur carbonaceous chondrites."[2]
Lonsdaleites Edit
"The mineral Lonsdaleite is a translucent, brownish yellow and is made from the atoms of carbon but the arrangement of these atoms is different from the arrangement of carbon atoms in a diamond. [...] The mineral is very rare and is formed naturally whenever [...] graphite containing meteorites fall on the earth and hit the surface."[3]
"Found in the Canyon Diablo and Goalpara meteorites."[2]
Fullerites Edit
Fullerite appears to be a tentative name for the mineral occurrence of buckyballs.
"By means of high-resoluton transmission electron microscopy, both C60 and C70 fullerenes have been found in a, carbon-rich Precambrian rock from Russia The fullerenes were confirmed by Fourier transform mass spectrometry with both laser desorption and thermal desorption/electron-capture methods to verify that the fullerenes were indeed present in the geological sample".[4]
Space carbons Edit
Apparently graphitic-like carbon particles such as shown in the image on the right have been found in space and brought back to Earth.
Organic minerals Edit
An organic mineral appears to be a naturally occurring mineral containing one or more organic chemicals at a concentration of greater than 25 molecular %.
Carpathites Edit
Carpathite (aka Karpatite) is a very rare organic species (C24H12).[2] It is a polycyclic aromatic hydrocarbon (PAH). This specimen is from the old Picacho Mercury Mine of California. It exhibits a radial spray of highly lustrous, canary-yellow carpathite lathes to 2.0 cm on drusy quartz. Another crossed cluster of crystals above reach 3.0 cm. It has 66.7 at % carbon.
Idrialites Edit
With a formula of C22H14,[2] idrialites are about 61 at % carbon.
Idrialite is "a complex natural mineral composed entirely of cata-condensed polyaromatic hydrocarbons (PAHs), usually containing a thiophenic or aliphatic five-membered ring."[5]
Idrialite "(and also curtisite) represents more complex mixtures of chain-type PAHs with molecular weights ranging from 216 to 372 amu [5]."[5]
"Some of the bands in the idrialite spectra are attributed to specific vibrational modes of thiophene or fluorene-type PAHs, especially in the region bellow 1000 cm−1. These modes at 495, 705 and 750 cm−1 along with C–H or C–H2 stretching modes around 3000 cm−1 can be then used to distinguish such groups of PAHs in complicated organic mineral mixtures like idrialite."[5]
Idrialite may include benzonaphthothiophenes (chemical formula: C16H10S).[5]
Kratochvilites Edit
Def. a "rare organic mineral [C14H10 or (C6H4)2CH2, a polymorph of fluorene], an orthorhombic hydrocarbon formed by combustion of coal or pyritic black shale deposits"[6] is called kratochvilite
Kratochvilites have about 58.3 at % carbon.
Moissanite Edit
Moissanite is native SiC.[2]
Hoelites Edit
Hoelites are 50 at % carbon with a formula of (C6H4)2(CO)2.[2]
Abelsonites Edit
Abelsonites have a chemical formula of NiC31H34N4, for 44.3 at % carbon.[2]
Simonellites Edit
Def. an "orthorhombic-dipyramidal white mineral containing carbon and hydrogen [C19H24]"[7] is called a simonellite.
Simonellites have about 44.2 at % carbon.
Hartites Edit
Hartites have about 37 at % carbon with a formula of C20H34.[2]
Fichtelites Edit
Def. a "rare white monoclinic organic mineral, [7-isopropyl-1,4a-dimethyl-dodecahydro-1H-phenanthrene (C19H34)],[8] found in fossilized wood"[9] is called a fichtelite.
Also, occurs in "fossilized pine wood from a peat bog; in organic-rich modern marine sediment."[10]
Fichtelites have about 35.8 at % carbon.
Evenkites Edit
Evenkite has about 32.4 at % carbon in its formula: (CH3)2(CH2)22.[2]
Hypotheses Edit
- The easiest resource for specific elements is as a native element mineral.
See also Edit
References Edit
- ↑ diamond. San Francisco, California: Wikimedia Foundation, Inc. October 16, 2012. http://en.wiktionary.org/wiki/diamond. Retrieved 2012-10-23.
- ↑ 2.0 2.1 2.2 2.3 2.4 2.5 2.6 2.7 2.8 2.9 Willard Lincoln Roberts; George Robert Rapp Jr.; Julius Weber (1974). Encyclopedia of Minerals. New York, New York, USA: Van Nostrand Reinhold Company. pp. 121-2.
- ↑ payam (30 July 2013). Top 10 Hardest Material in the world. Help Tips. http://helptips.net/26/top-10-hardest-material-in-the-world/. Retrieved 2015-07-30.
- ↑ Peter R. Buseck; Semeon J. Tsipursky; Robert Hettich (10 July 1992). "Fullerenes from the Geological Environment". Science 257 (5067): 215-7. doi:10.1126/science.257.5067.215. http://www.sciencemag.org/content/257/5067/215. Retrieved 2015-07-30.
- ↑ 5.0 5.1 5.2 5.3 Otakar Frank; Jan Jehlička; Howell G.M. Edwards (15 December 2007). "Raman spectroscopy as tool for the characterization of thio-polyaromatic hydrocarbons in organic minerals". Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 68 (4): 1065–9. doi:10.1016/j.saa.2006.12.033. http://www.sciencedirect.com/science/article/pii/S1386142506007621. Retrieved 2015-11-02.
- ↑ Equinox (27 October 2008). kratochvilite. San Francisco, California: Wikimedia Foundation, Inc. https://en.wiktionary.org/wiki/kratochvilite. Retrieved 2015-01-09.
- ↑ Equinox (4 September 2011). simonellite. San Francisco, California: Wikimedia Foundation, Inc. https://en.wiktionary.org/wiki/simonellite. Retrieved 2015-01-09.
- ↑ SemperBlotto (15 March 2014). fichtelite. San Francisco, California: Wikimedia Foundation, Inc. https://en.wiktionary.org/wiki/fichtelite. Retrieved 2015-01-09.
- ↑ Equinox (28 September 2010). fichtelite. San Francisco, California: Wikimedia Foundation, Inc. https://en.wiktionary.org/wiki/fichtelite. Retrieved 2015-01-09.
- ↑ R. Ruff (2005). Fichtelite. Mineral Data Publishing. http://rruff.info/doclib/hom/fichtelite.pdf. Retrieved 2015-01-09.