| _version_ | 1867170034485297152 |
|---|---|
| author | Furbish, William J Schrader, Ed L |
| author_facet | Furbish, William J Schrader, Ed L |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A variety of secondary minerals, formed in response to different oxidation and hydration states, are found in vugs and on fracture surfaces of the basalt cores from DSDP Leg 54. The minerals are smectite (blue to grey), high-magnesium calcite, manganoan calcite, aragonite, iron oxides, phillipsite, todorokite, marcasite, and hydrobiotite. The relationship of the mineral assemblages to four depositional modes of the basalts are delineated. A definite sequence and genetic link exists between mineral type and host rock which is dependent upon the origin and subsequent cooling history of the basalt. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_823555 |
| institution | PANGAEA |
| language | en |
| publishDate | 1980 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Minerals found in vesicles and fractures from DSDP Leg 54 Holes basalts Furbish, William J Schrader, Ed L 54-420; 54-421; 54-422; 54-423; 54-424; 54-425; 54-427; 54-428; 54-428A; 54-429A; Aragonite; Calcite; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg54; Longitude of event; Minerals; North Pacific/CONT RISE; North Pacific/MOUND; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/TROUGH; Oxides; Piece; Sample code/label; Smectite; X-ray diffraction (XRD) A variety of secondary minerals, formed in response to different oxidation and hydration states, are found in vugs and on fracture surfaces of the basalt cores from DSDP Leg 54. The minerals are smectite (blue to grey), high-magnesium calcite, manganoan calcite, aragonite, iron oxides, phillipsite, todorokite, marcasite, and hydrobiotite. The relationship of the mineral assemblages to four depositional modes of the basalts are delineated. A definite sequence and genetic link exists between mineral type and host rock which is dependent upon the origin and subsequent cooling history of the basalt. |
| title | (Table 1) Minerals found in vesicles and fractures from DSDP Leg 54 Holes basalts |
| topic | 54-420; 54-421; 54-422; 54-423; 54-424; 54-425; 54-427; 54-428; 54-428A; 54-429A; Aragonite; Calcite; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg54; Longitude of event; Minerals; North Pacific/CONT RISE; North Pacific/MOUND; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/TROUGH; Oxides; Piece; Sample code/label; Smectite; X-ray diffraction (XRD) |
| url | https://doi.org/10.1594/PANGAEA.823555 |