Donate now to keep alive!Help|Log In|Register|
Home PageMindat NewsThe Mindat ManualHistory of MindatCopyright StatusManagement TeamContact UsAdvertise on Mindat
Donate to MindatSponsor a PageSponsored PagesTop Available PagesMindat AdvertisersAdvertise on Mindat
The most common minerals on earthMineral PhotographyThe Elements and their Minerals
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralSearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
StatisticsThe ElementsMember ListBooks & MagazinesMineral MuseumsMineral Shows & EventsThe Mindat DirectoryDevice Settings
Photo SearchPhoto GalleriesNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day Gallery

Stannite, Kesterite, Owyheeite and other Yaogangxian friends

Last Updated: 6th Oct 2012

By Jean-Francois Carpentier

This one is a quite complicated specimen, illustrating the rich mineralogy/chemistry that took place at Yaogangxian.

The specimen (overall 6.0 x 3.0 x 3.0 cm) features sharp tetrahedrons, highly lustrous, with a dark bronze olive color or brown-black color on edges. Some of these crystals – or more precisely some parts of these crystals, actually the stepped edges of these tetrahedrons –, are made of Sphalerite (the black brown looking one), which is most probably the mineral that originally built up.

However, many of these crystals have an hollow structure and are apparently completely pseudo(para)morphosed to Stannite (the bronze olive mineral).

EDS and single-crystal XRD analyses revealed that Stannite is the main pseudo(para)morphosis phase
average composition: Cu1.71(Fe0.76,Zn0.13)sum=0.89Sn0.98S4;
unit cell parameters determined at 298 K: group I-42m, a = 5.46, c = 10.74 Å; this rules out Ferrokesterite

EDS spectrum of Stannite (main phase component)

Yet another intermediary member between Kesterite and Stannite, with an average formula Cu1.70(Fe0.54,Zn0.39)sum=0.93Sn0.98S4, is also associated to this main phase;
EDS spectrum of intermediary member in between stannite and kesterite (minor phase component)

Very small overgrowths of Galena are also present on this Stannite-Kesterite assemblage. This can be visualized in the SEM image below.

Detail of a Stannite crystal showing “tetrahedral” overgrowths of Galena; Stannite is the dark grey phase; the small lighter domains on this phase are an intermediary member between Kesterite and Stannite
Main grey phase: Stannite;
Inclusions: intermediary member between Kesterite and Stannite;
Large white crystals: Galena

Finally, the specimen revealed the presence of Bournonite (grey masses to ca. 1 cm, “frozen” in the matrix, EDS confirmed) as well as two more species which were found as small needles (to a few mm) in a little vug nested in between the tetrahedral crystals: Boulangerite (EDS and XRD confirmed) and, more interestingly, Owyheeite (XRD and EDS confirmed; average formula: Ag3.3Pb8.3Sb10.9S28). This seems to be the first identification of Owyheeite at Yaogangxian.

Many thanks to Robert Cohen for the gift of this specimen (another larger one is in his hands) and to Bert Ottens for fruitful discussions on this very specimen and the most interesting mineralogy of Yaogangxian deposits.

Article has been viewed at least 6867 times.


In order to leave comments to this article, you must be registered
Mineral and/or Locality is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © and the Hudson Institute of Mineralogy 1993-2017, except where stated. relies on the contributions of thousands of members and supporters.
Privacy Policy - Terms & Conditions - Contact Us Current server date and time: November 24, 2017 13:00:17
Go to top of page