Skip to content
Surf Wiki
Save to docs
general/sulfide-minerals

From Surf Wiki (app.surf) — the open knowledge base

Getchellite


FieldValue
nameGetchellite
categorySulfide mineral
boxwidth24
imageGetchellite.jpg
imagesize260px
captionGetchellite from Khaidarkan, Fergana Valley, Osh Oblast, Kyrgyzstan. Specimen size 3.6 cm.
molweight293.81 g/mol
formulaAsSbS3
IMAsymbolGet
strunz2.FA.35
dana2.11.1.2
systemMonoclinic
classPrismatic (2/m)
(same H-M symbol)
symmetryP21/a
colorDark red, sometimes with a purple to green iridescent tarnish
habitSubhedral crystals and massive with a platy texture
twinningSimple and polysynthetic twins with the twin plane and composition plane parallel to {001}
cleavagePerfect on {001}
fractureSplintery
tenacitySectile; cleavage flakes are flexible and inelastic
mohs1.5 to 2
lusterVitreous to pearly on cleavage surfaces, otherwise resinous
refractiven = 2.720. Dispersion r v strong
opticalpropBiaxial (+), 2V=46°
streakOrange red
gravity3.92 (observed) 4.0 (calculated)
melt340 °C to 355 °C
diaphaneityTransparent
otherNot radioactive
references

(same H-M symbol)

Getchellite is a rare sulfide of arsenic and antimony, AsSbS3, that was discovered by B. G. Weissberg of the New Zealand Department of Scientific and Industrial Research in 1963, and approved as a new species by the International Mineralogical Association in 1965. Many metal sulfides are grey to black, but a few are brightly colored. Orpiment is yellow to brownish gold, cinnabar is deep red and getchellite is a bright orange red.

Thermal properties

Getchellite turns darker red when heated, becoming black by the time it reaches its melting point. Close to this temperature it sublimes (changes directly from a solid to a vapor) and recrystallizes on cooler surfaces as minute acicular black crystals. Melting point: 340 °C to 355 °C. Boiling point: near 470 °C.

Structure

Each of the semimetal atoms, arsenic and antimony, is bonded to three sulfur atoms to form a trigonal pyramid characteristic of elements in group V of the periodic table. These pyramids form 8-membered rings which in turn combine to form sheets parallel to (001), with each sulfur atom bonded to two semimetal atoms. The occupancy of the metal sites is disordered, and within the sheets the 8-membered rings are orientated normal to the plane of the sheet. The sheet structure is responsible for the cleavage and twin planes of getchellite Unit cell a = 11.949 Å; b = 9.028 Å; c = 10.130 Å; β= 116.15°; V = 980.9 Å3; Z = 8.

Powder diffraction

X-Ray Powder Diffraction:
d spacing
relative intensity

Discovery

In August 1962 Weissberg visited the Getchell mine at Adam Peak, about 32 km northeast of Golconda, in Humboldt County, Nevada, US. The purpose of his visit was to collect samples for a study of the relationship between various fairly common sulfides, not to look for new minerals. Getchellite was in some of the samples, but it was not discovered until the rocks were re-examined, a year later. The new mineral was named after the Getchell Mine, which in turn became the type locality.

Environment

At the type locality getchellite is found in an epithermal (formed at low temperature) arsenical gold deposit in a narrow, steeply dipping fault zone cutting across interbedded shales, argillites (lithified muds and oozes) and limestones, near an intrusion of granodiorite. Associated minerals are orpiment, realgar, stibnite, cinnabar and quartz, as well as galkhaite, laffittite, chabournéite, christite, lorandite, marcasite, barite, fluorite and calcite.

Distribution

Getchellite is found at the type locality in Nevada, United States, and also in Azerbaijan, China, Iran, Japan, Kyrgyzstan and Russia.

Synthesis

Getchellite has been synthesized from As3SbS6 glass in sodium sulfide solutions at 2600 C. and 1,000 bars pressure.

References

References

  1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
  2. "Getchellite Mineral Data".
  3. http://www.mindat.org/min-1686.html Mindat.org
  4. http://rruff.geo.arizona.edu/doclib/hom/getchellite.pdf Handbook of Mineralogy
  5. Weissberg, B G, American Mineralogist (1965) Volume 50 pages 1817 to 1826
  6. (2004). "Structural reinvestigation of getchellite As0.98Sb1.02S3.00". American Mineralogist.
  7. (November 1973). "The crystal structure of getchellite, AsSbS3". Acta Crystallographica.
  8. Space group P21/a.Gaines et Al (1997) Dana's New Mineralogy Eighth Edition, Wiley
  9. "Mineral Sciences Collections Search".
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

Want to explore this topic further?

Ask Mako anything about Getchellite — get instant answers, deeper analysis, and related topics.

Research with Mako

Free with your Surf account

Content sourced from Wikipedia, available under CC BY-SA 4.0.

This content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.

Report