| _version_ | 1867171842948595712 |
|---|---|
| author | Simons, FS Straczek, J A |
| author_facet | Simons, FS Straczek, J A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Deposits of manganese ore have been found in five of the six provinces of Cuba and have been reported from the sixth. Only Oriente and Pinar del Rio provinces have more than a few known deposits and only the deposits of Oriente have yielded any appreciable amount of ore. In this area the Cobre formation, of late Cretaceous(?) to middle Eocene age, overlies the Vinent formation but their stratigraphie relations are unknown. The Cobre overlies unconformably the Habana(?) formation. The Cobre formation consists of andesitic, basaltic, and dacitic tuff, agglomerate, and lavas with minor amounts of marine clastic and limestone deposits, and a prominent limestone bed, the Charco Redondo limestone member, at the top of the formation. All productive manganese deposits of Oriente are in the Cobre formation, usually within a few tens of meters above or below the base of the Charco Redondo limestone member. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_866860 |
| institution | PANGAEA |
| language | en |
| publishDate | 1958 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Description of manganese deposits from the Oriente province in Cuba Simons, FS Straczek, J A Charco_Redondo_S; Comment; Cuba; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Guanaba_S; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Ponupo_S; Position; Quantity of deposit; Quinto_S; Sample ID; Sediment type; Size; Substrate type; Taratana_S Deposits of manganese ore have been found in five of the six provinces of Cuba and have been reported from the sixth. Only Oriente and Pinar del Rio provinces have more than a few known deposits and only the deposits of Oriente have yielded any appreciable amount of ore. In this area the Cobre formation, of late Cretaceous(?) to middle Eocene age, overlies the Vinent formation but their stratigraphie relations are unknown. The Cobre overlies unconformably the Habana(?) formation. The Cobre formation consists of andesitic, basaltic, and dacitic tuff, agglomerate, and lavas with minor amounts of marine clastic and limestone deposits, and a prominent limestone bed, the Charco Redondo limestone member, at the top of the formation. All productive manganese deposits of Oriente are in the Cobre formation, usually within a few tens of meters above or below the base of the Charco Redondo limestone member. |
| title | Description of manganese deposits from the Oriente province in Cuba |
| topic | Charco_Redondo_S; Comment; Cuba; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Guanaba_S; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Ponupo_S; Position; Quantity of deposit; Quinto_S; Sample ID; Sediment type; Size; Substrate type; Taratana_S |
| url | https://doi.org/10.1594/PANGAEA.866860 |