File:Pyrrhotite crystal (Dalnegorsk Skarn Deposit, Late Cretaceous, 70-90 Ma; Dalnegorsk, Russia) 3.jpg
![File:Pyrrhotite crystal (Dalnegorsk Skarn Deposit, Late Cretaceous, 70-90 Ma; Dalnegorsk, Russia) 3.jpg](https://upload.wikimedia.org/wikipedia/commons/thumb/4/47/Pyrrhotite_crystal_%28Dalnegorsk_Skarn_Deposit%2C_Late_Cretaceous%2C_70-90_Ma%3B_Dalnegorsk%2C_Russia%29_3.jpg/728px-Pyrrhotite_crystal_%28Dalnegorsk_Skarn_Deposit%2C_Late_Cretaceous%2C_70-90_Ma%3B_Dalnegorsk%2C_Russia%29_3.jpg?20201214193705)
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[edit]DescriptionPyrrhotite crystal (Dalnegorsk Skarn Deposit, Late Cretaceous, 70-90 Ma; Dalnegorsk, Russia) 3.jpg |
English: Pyrrhotite crystal from the Cretaceous of Russia.
A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5600 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates. The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals. Pyrrhotite is imperfect iron monosulfide (Fe(1-x)S). The atomic structure of pyrrhotite has holes due to an insufficient number of iron atoms, cf. sulfur atoms. Iron monosulfide is a common, but minor, component of many meteorites, but it lacks the atomic-scale “holes” of pyrrhotite, and is called troilite (FeS). Pyrrhotite is superficially like pyrite in appearance and chemistry, but they are different minerals. Pyrrhotite has a metallic luster, a brownish-brassy or bronzish color, a black streak, no cleavage, and sticks to a magnet. What’s particularly distinctive about pyrrhotite is that it is variably magnetic. The holes in the atomic structure gives pyrrhotite its magnetism. But, there's variation in the number of missing iron atoms from sample to sample, so pyrrhotite ends up having variable magnetism. More holes results in stronger magnetism. Few holes results in weaker magnetism. The beautiful hexagonal crystal of pyrrhotite seen here comes from a polymetallic sulfide ore body at the famous Dalnegorsk Skarn Deposit in Russia. The deposit consists of mineral-filled solution cavities in Triassic limestones that have been intruded by Late Cretaceous granodiorites. The skarn zone itself has been intruded by 64 Ma granite. Geologic unit: Dalnegorsk Skarn Deposit, Late Cretaceous, 70-90 Ma Locality: Nikolaevskiy Mine, Dalnegorsk, southern Sikhote-Alin Mountains, Maritime Region ("Primorskiy Kray"), far-eastern Russia (apparently in the vicinity of 44° 33' 09.48" North latitude, 135° 35' 00.19" East longitude) Photo gallery of pyrrhotite: www.mindat.org/gallery.php?min=3328 |
Date | |
Source | https://www.flickr.com/photos/47445767@N05/50713741497/ |
Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/50713741497. It was reviewed on 14 December 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
14 December 2020
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current | 19:37, 14 December 2020 | ![]() | 2,193 × 1,806 (3.57 MB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50713741497/ with UploadWizard |
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Camera manufacturer | Canon |
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Camera model | Canon PowerShot D10 |
Exposure time | 1/500 sec (0.002) |
F-number | f/3.5 |
ISO speed rating | 80 |
Date and time of data generation | 19:45, 11 December 2020 |
Lens focal length | 9.681 mm |
Width | 4,000 px |
Height | 3,000 px |
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Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 180 dpi |
Vertical resolution | 180 dpi |
Software used | Adobe Photoshop Elements 18.0 (Macintosh) |
File change date and time | 06:10, 13 December 2020 |
Y and C positioning | Co-sited |
Exif version | 2.21 |
Date and time of digitizing | 19:45, 11 December 2020 |
Meaning of each component |
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APEX aperture | 3.625 |
APEX exposure bias | −0.33333333333333 |
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Flash | Flash did not fire, compulsory flash suppression |
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Focal plane resolution unit | inches |
Sensing method | One-chip color area sensor |
File source | Digital still camera |
Custom image processing | Normal process |
Exposure mode | Manual exposure |
White balance | Auto white balance |
Digital zoom ratio | 1 |
Scene capture type | Standard |
Lens used | 6.2-18.6 mm |
Date metadata was last modified | 01:10, 13 December 2020 |
Unique ID of original document | AF890B078A2ADAE642FF84F69F35F4BC |
IIM version | 24,576 |