|
|
Nováčekite-II
This page is currently not sponsored. Click here to sponsor this page.
| Formula: |
| |||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| System: | Monoclinic | |||||||||||||||||||||||
See nováčekite and nováčekite-I.
Nováčekite-I is very unstable under ambient conditions and quickly dehydrates to nováčekite-II, in part also to metanováčekite.
Nováčekite-II may also reversibly rehydrate from metanováčekite under ambient conditions.
Classification of Nováčekite-II | ||||||||||||||||||||||
| IMA status: | Valid - first described prior to 1959 (pre-IMA) - "Grandfathered" | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mindat.org URL: | http://www.mindat.org/min-39584.html Please feel free to link to this page. | |||||||||||||||||||||
Crystallography of Nováčekite-II | ||||||||||||||||||||||
| Crystal System: | Monoclinic | |||||||||||||||||||||
| Class (H-M): | 2/m - Prismatic | |||||||||||||||||||||
| Cell Parameters: | a = 7.1328(11) Å, b = 20.085(3) Å, c = 7.1569(11) Å β = 90.585(3)° | |||||||||||||||||||||
| Ratio: | a:b:c = 0.355 : 1 : 0.356 | |||||||||||||||||||||
| Unit Cell Volume: | V 1,025.26 ų (Calculated from Unit Cell) | |||||||||||||||||||||
| Comment: | SG P21/n; pseudotetragonal ((pseudo-space group P42/n, a = 7.18-7.20 A, c = 20.16-20.22 A, Z = 2). | |||||||||||||||||||||
Chemical Properties of Nováčekite-II | ||||||||||||||||||||||
| Formula: |
| |||||||||||||||||||||
| Essential elements: | As, H, Mg, O, U | |||||||||||||||||||||
| All elements listed in formula: | As, H, Mg, O, U | |||||||||||||||||||||
Other Information | ||||||||||||||||||||||
| Health Warning: | No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care. | |||||||||||||||||||||
References for Nováčekite-II | ||||||||||||||||||||||
| Reference List: - + | Walenta, K. & Wimmenauer, W. (1961): Der Mineralbestand des Michaelganges im Weiler bei Lahr (Schwarzwald). Jh. Geol. Landesamt Baden-Württemberg, 4, 7-37. Walenta, K. (1964): Rare arsenate minerals with special consideration of occurrences in the Black Forest. Mineral. Petrog. Mitt. 9, 111-174. (in German). Locock, A. J., Burns, P. C. & Flynn, T. M. (2004): Divalent transition metals and magnesium in structures that contain the autunite-type sheet. Canadian Mineralogist 42, 1699-1718. | |||||||||||||||||||||
Internet Links for Nováčekite-II | ||||||||||||||||||||||
| Search Engines: |
| |||||||||||||||||||||
| External Links: | ||||||||||||||||||||||
| Mineral Dealers: | ||||||||||||||||||||||
| Jobs: | ||||||||||||||||||||||
Localities for Nováčekite-II | ||||||||||||||||||||||
|
The map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the
symbol to view information about a locality.
The symbol next to localities in the list
can be used to jump to that position on the map.
| ||||||||||||||||||||||
(TL) indicates type locality. ? indicates mineral may be doubtful at this locality. All other localities listed without reference should be considered as uncertain and unproven until references can be found.
|
Mindat Lightbox
Options| Fade toolbar when not in focus | Fix toolbar to bottom of page | ||
|---|---|---|---|
| Hide Social Media Links | |||
| Slideshow frame delay | seconds | ||
Updated Mineral Entry: Schlüterite-(Y) From Uwe Kolitsch, 23rd May 2013 07:31:28

symbol to view information about a locality.
The 













