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PhotosChalcocite - Steward Mine, Butte, Butte District, Silver Bow Co., Montana, USA
10th Jul 2017 22:46 UTCRichard Gunter Expert
12th Jul 2017 06:17 UTCRob Woodside 🌟 Manager
12th Jul 2017 15:39 UTCRichard Gunter Expert
These look more like octahedrons but are unlike any of the photographed Pyrite from the Butte area. The staining of Pyrite with secondary Cu sulphides in the Butte Chalcocite-Bornite-Digenite samples makes colour determination difficult, even on broken surfaces. They certainly look like very strange Pyrites.
13th Jul 2017 16:08 UTCRob Woodside 🌟 Manager
13th Jul 2017 16:14 UTCRichard Gunter Expert
I think so as well. I will have a look to see what I want to sample from it.
13th Jul 2017 22:43 UTCRichard Gunter Expert
I was investigating the pyrite crystals and found that several of the octahedral faces have isosceles triangular growth figures centered on the octahedral face rather than striations. The terminations of the triangles point to the center of the adjacent large edge. I did not think pyrite's crystal system allowed for this, does it? I have seen something similar on carrolite, where the triangular growth figures point to the junction of the large faces and on tetrahedrite but never on pyrite.
17th Jul 2017 19:12 UTCRob Woodside 🌟 Manager
17th Jul 2017 19:46 UTCRichard Gunter Expert
I have checked the crystallography and the only one that has this kind of growth feature is the Tetrahedrite Group, including Colusite. I have found identical growth features on my Tetrahedrite sample from Pachapaqui, Peru where triangular growth features occur with apacies intersecting the crystal faces. Interestingly the Tetrahedrite also contains triangular growth features that intersect the crystal edges but these triangles are 180 degrees to the first set.
I have not seen any report on these triangular growth features on Colusite. I will try to post a photo but it will be challenging.
17th Jul 2017 22:13 UTCRichard Gunter Expert
A diagram of the triangular growth features on an octahedral pyrite is from a Travesella pyrite in Dana's Elements of Mineralogy. The diagram indicates that the apex of the triangles will subtend a 33 degree or 66 degree angle to the octahedral crystal edge. Sometimes you need the old data as modern mineralogy often does not look at these things. I checked my Musen Siegenite and its triangular growth features are identical to the Carrolite, as they should be.
18th Jul 2017 00:12 UTCRichard Gunter Expert
18th Jul 2017 00:29 UTCRobert Rothenberg
Bob
18th Jul 2017 09:30 UTCRob Woodside 🌟 Manager
18th Jul 2017 15:27 UTCRichard Gunter Expert
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Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 23, 2024 17:01:04