| Display title | Chemistry:Sulfate minerals |
| Default sort key | Sulfate minerals |
| Page length (in bytes) | 16,328 |
| Namespace ID | 3022 |
| Namespace | Chemistry |
| Page ID | 824834 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
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| Counted as a content page | Yes |
| Page image |  |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>WikiEd2 |
| Date of page creation | 02:46, 6 February 2024 |
| Latest editor | imported>WikiEd2 |
| Date of latest edit | 02:46, 6 February 2024 |
| Total number of edits | 1 |
| Recent number of edits (within past 90 days) | 0 |
| Recent number of distinct authors | 0 |
Description | Content |
Article description: (description)
This attribute controls the content of the description and og:description elements. | The sulfate minerals are a class of minerals that include the sulfate ion (SO42−) within their structure. The sulfate minerals occur commonly in primary evaporite depositional environments, as gangue minerals in hydrothermal veins and as secondary minerals in the oxidizing zone of sulfide mineral deposits... |
