| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | The early Tertiary deep-water sandstones near San Sebastian, Spain; some aspects of diagenesis |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Knox, G. J. | Author |
|---|
| Year | 1976 (July) | Volume | 113 |
|---|
| Issue | 4 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800047610Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 251177 | Long-form Identifier | mindat:1:5:251177:5 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Knox, G. J. (1976) The early Tertiary deep-water sandstones near San Sebastian, Spain; some aspects of diagenesis. Geological Magazine, 113 (4) 341-348 doi:10.1017/s0016756800047610 |
|---|
| Plain Text | Knox, G. J. (1976) The early Tertiary deep-water sandstones near San Sebastian, Spain; some aspects of diagenesis. Geological Magazine, 113 (4) 341-348 doi:10.1017/s0016756800047610 |
|---|
| In | (1976, July) Geological Magazine Vol. 113 (4) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | SummaryNear San Sebastian, northern Spain, are outcrops of a system of deep-water fans deposited beyond the mouth of a submarine canyon from southward flowing currents. The sandstones consist of mixed siliciclastic detritals and carbonate fragments. The latter includes a derived heterogeneous marine fauna. Carbonate content varies and has played a major part in diagenesis. Early cementation by limited quartz and to a greater extent calcite involved local expansion. Later compaction has led to prominent pressure-solution phenomena of calcite and quartz with formation of microstylolites. Leaching owing to weathering has led to removal of some carbonate and formation of kaolinite from micas. |
|---|
These are possibly similar items as determined by title/reference text matching only.
