| Deposit ID | 10400371 |
|---|---|
| Record type | Deposit |
| Current site name | Nama Retention License |
| Geographic coordinates: | 27.51549, -12.19783 (WGS84) |
|---|
Political divisions (FIPS codes)
Zambia(country)
Africa(continent)
Land(continent)
| Country |
|---|
| Zambia |
| Materials | Type of material |
|---|---|
| Magnetite | Ore |
| Pyrite | Ore |
| Chalcopyrite | Ore |
| Hematite | Ore |
| Chlorite | Gangue |
| Talc | Gangue |
| Epidote | Gangue |
| Silica | Gangue |
| Hematite | Gangue |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock |
| Rock type qualifier | mixtite |
| Rock unit name | Kundulungu Group |
| (1) | 27.51549, -12.19783 |
|---|
| Operation type | Surface |
|---|---|
| Development status | Prospect |
| Significant | Yes |
| Type | In-situ |
|---|---|
| Name | Nama D |
| Estimate year | 2008 |
| Total resources | 63909000mt ore |
| Remarks | Indicated + Inferred = 63,909,000 @ 0.035% Cu and 0.0802% Co |
| Type | In-situ | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Name | Nama Anomaly C, indicated | ||||||||||||||||||||||||||||
| Estimate year | 2007 | ||||||||||||||||||||||||||||
| Indicated | 78218000mt | ||||||||||||||||||||||||||||
| Remarks | Nama Anomaly C has indicated resource of 78,218,000 mt @ 0.012% cu and 0.043% Co. Based on 73 drill holes. (Grant and Haslett, 2007). | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Type | In-situ |
|---|---|
| Name | Nama A |
| Estimate year | 2008 |
| Indicated | 43656000mt ore |
| Remarks | @ 0.099% Cu and 0.055% Co |
Grant, David, and Haslett, Michael, 2007, Independent competent persons report of the Nama retention license in northern Zambia and held by Caledonian Mining Limited, May 1, 2007, 67 p. [available from sedar.com, Caledonia Mining Corporation, May 7, 2007, Technical report (NI-43-101) - English as of 5/26/10]. p. 58.
ACP Mining Data Bank [Secretariat of the African and Caribbean and Pacific Group of States Group], undated, http://mines.acp.int/html/mine_ZMB-00088_en.html
Grant, David, 2008, Independent Qualified Person Report for Resource Body D in the Nama Retention Licence[sic], Northern Zambia: Report prepared for Caledonia Mining Corp and Caledonia Nama Ltd, (dated May 1, 2008), 51 p. (Available for download at www.sedar.com [Caledonia Mining Corporation, Technical report (NI-43-101) - English, filed May 2, 2008]).
| Subject category | Comment text |
|---|---|
| Deposit | Deposit is NOT of the sed-hosted Cu type. |
| Deposit | From Tim Hayes, Jan 22, 2010: "NAMA was classified as not sed-hosted copper, because it does not fit the overall sediment-hosted strata-bound Cu model on a number of counts: (1) the resource number is associated with body of epigenetic hematite and magnetite, not with any type of reduced rock that is carbonaceous or pyritic nearby, (2) copper grades are 0.05%; that's no copper deposit of any kind in my book; the values at Nama are mostly in Co, but that too is not all that great: 0.08%; certainly adding something that is 0.05% Cu is going to be an extreme outlier on any grade model; (3) these values are associated with the body described as taking the aspect of an antiform that cuts across stratigraphy up in the Mwashya Fm., It certainly isn't stratiform, therefore, and it is questionable from current knowledge whether is is strata-bound, though as currently described, it could be. There is one more described body of oxide-hosted cobalt-anomalous rock around in the CACB. It is NNE of Musoshi and WNW of Kinsenda hosted in Lefebvre's Kalumbalesa Group (basal conglomeratic clastics of the Katangan Supergroup; most from Zambia would make this part of the Mindola Clastics Formation. Others who have worked in the SE part of the Copperbelt in DRC would name it Chimfunsi Fm. It is clearly down section from either the Copperbelt Orebody Member and probably down section from R.A.T. It might correlate with the basal conglomerates of the Katangan of the Nzilo, DRC, area.). The hematite mineralization near Kalumbalesa, DRC, averages 16 ppm Cu and 82 ppm Co. Thus the Co is anomalous, though 10X less concentrated than at Nama. The Cu is not even anomalous. (4) Last but not least; the plunging antiformal hematite-magnetite mineralization is open to the north." |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 04-JUN-10 | Wilson, Anna B. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.