| Locality type: | Mine |
| Classification |
|---|
|
| Species: | 'Svanbergite-Woodhouseite Series' (not an IMA approved species) |
| Confirmation |
|---|
|
| Validity: | Believed Valid |
| Data |
|---|
|
| Mineral Data: | Click here to view Svanbergite-Woodhouseite Series data |
| Locality Data: | Click here to view La Providencia Mine, Cajamarca District, Cajamarca Province, Cajamarca, Peru |
| Data Identifiers |
|---|
|
| Mindat Occurrence Record ID: | 599418 |
| Long-form Identifier: | 1:3:599418:2 |
| GUID (UUID V4): | ee894fcf-1e8f-4da8-ae15-6bcd1b4ecfcf |
| References |
|---|
|
Dill, H.G., Bosse, H.-R., Henning, K.-H., Fricke, A., and Ahrendt, H. (1997): Mineralium Deposita 32, 149-163. |
| Reference Search (possible matching items) |
|---|
 | Dill, H. G., Bosse, H.-R., Henning, K.-H., Fricke, A., Ahrendt, H. (1997) Mineralogical and chemical variations in hypogene and supergene kaolin deposits in a mobile fold belt the Central Andes of northwestern Peru. Mineralium Deposita, 32 (2) 149-163 doi:10.1007/s001260050081 | Journal (article/letter/editorial) | | northwestern Peru Received: 11 August 1995 / Accepted: 8 May 1996 Abstract In western Peru kaolin-alunite...REE-bearing svanbergite and florencite originate from supergene alteration. Woodhouseite, goyazite, crandallite...crandallite and pure svanbergite develop in hypogene and supergene kaolin deposits. The distinction between... S, Zr vs. Ti, Cr + Nb vs. Ti + Fe, and Ce + Y + La vs. Ba + Sr). S, Ba, and Sr are considerably enriched...1984; Mitchell 1992). The clay deposits in western Peru permit discrimination of hypogene and supergene |
|
