|
Albite  | |
| | Reference: | [MinRec 11:370; Rocks & Min.:63:49 & 53.] |
| |
|
|
Albite var: Cleavelandite  | |
| | Reference: | [MinRec 11:370] |
| |
|
|
Amblygonite  | |
| | Reference: | [MinRec 11:370] |
| |
|
|
Beryl  | |
| |
|
Cassiterite  | |
| | Reference: | [MinRec 11:370; Rocks & Min.:63:49 & 53.] |
| |
|
|
Coeruleolactite  | |
| | Reference: | [Cassedanne, J.P & J.O. (1980): Famous mineral localities: The Cruzeiro mine, past and present. Mineralogical Record 11: 363-367 +370] |
| |
|
|
'Columbite-Tantalite'  | |
| | Reference: | [MinRec 11:370] |
| |
|
|
Cookeite  | |
| |
|
Elbaite  | | [Na][(Li,Al) | | ][Al | | ][(OH) | | |OH|(BO | | ) | | |Si | | O | | ] |
|
| | Reference: | [www.johnbetts-fineminerals.com]/ Cassedanne, J.P & J.O. (1980): Famous mineral localities: The Cruzeiro mine, past and presnet. Mineralogical Record 11: 363-367 +370; Dutrow, B. and Henry, D. J. (2000) Complexly zoned fibrous tourmaline: A record of evolving magmatic and hydrothermal fluids. Canadian Mineralogist, 38, 131-143.] |
| |
|
|
Foitite  | | [ ][Fe | | (Al,Fe | | )][Al | | ][(OH) | | |OH|(BO | | ) | | |Si | | O | | ] |
|
| | Reference: | [CanMin 38: 1399-1408 (2000); Dutrow, B. and Henry, D. J. (2000) Complexly zoned fibrous tourmaline: A record of evolving magmatic and hydrothermal fluids. Canadian Mineralogist, 38, 131-143.] |
| |
|
|
'Garnet Group'  | | X | | Z | | (TO | | ) | | (X = Ca, Fe, etc·, Z = Al, Cr, etc·, T = Si, As, V) |
|
| | Reference: | [MinRec 11:370] |
| |
|
|
'K Feldspar'  | |
| | Reference: | [Morteani, G., Preinfalk, C., and Horn, A.H. (2000): Mineralium Deposita 35, 638-655.] |
| |
|
|
Lepidolite  | |
| | Reference: | [CanMin 38: 1399-1408 (2000)] |
| |
|
|
Montmorillonite  | | (Na,Ca) | | (Al,Mg) | | Si | | O | | (OH) | | ·nH | | O |
|
| | Reference: | [MinRec 11:370] |
| |
|
|
Muscovite  | |
| | Reference: | [Morteani, G., Preinfalk, C., and Horn, A.H. (2000): Mineralium Deposita 35, 638-655.] |
| |
|
|
Petalite  | |
| | Reference: | [CanMin 38: 1399-1408 (2000)] |
| |
|
|
Phosphuranylite  | |
| | Reference: | [MinRec 11:370] |
| |
|
|
'Planerite-Turquoise Series'  | |
| | Description: | Originally reported to be coeruleolactite. All purported coeruleolactite examined by the authors of the 1998 report (Foord, E.E. & Taggart, J.E.) were largely Planerite, or Occasionally turquoise. Published analysis indicates that the vacany in the 'A' site is between 0.51-0.54 atom fraction, the balance in Cu-0.40 and Zn-0.06 to 0.09. It is suggested by this analysis that the turquoise structure likely cannot accomodate Ca in the 'A' site. | | Reference: | [Foord, E.E. & Taggart, J.E. (1998): A reexamination of the turquoise group; the mineral aheylite, planerite (redefined), turquoise and coeruleolactite. Mineralogical Magazine, 62, 93-111.] |
| |
|
|
Quartz  | |
| |
|
Quartz var: Smoky Quartz  | |
| |
|
Schorl  | | [Na][Fe | | ][Al | | ][(OH) | | |OH|(BO | | ) | | |Si | | O | | ] |
|
| | Reference: | [CanMin 38: 1399-1408 (2000); Dutrow, B. and Henry, D. J. (2000) Complexly zoned fibrous tourmaline: A record of evolving magmatic and hydrothermal fluids. Canadian Mineralogist, 38, 131-143.] |
| |
|
|
Spodumene  | |
| | Reference: | [MinRec 11:370] |
| |
|
|
Torbernite  | |
| | Reference: | [MinRec 11:370] |
| |
|
|
'Tourmaline var: Rubellite'  | |
| |
|
'Unnamed (F-analogue of elbaite)'  | |
| | Reference: | [Dutrow, B. and Henry, D. J. (2000) Complexly zoned fibrous tourmaline: A record of evolving magmatic and hydrothermal fluids. Canadian Mineralogist, 38, 131-143.] |
| |
|