| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Some Unusual Structures in Rhaetic Sandstones, near Cowbridge, Glamorgan |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Thomas, Trevor M. | Author |
|---|
| Year | 1951 (December) | Volume | 88 |
|---|
| Issue | 6 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800069958 |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 248103 | Long-form Identifier | mindat:1:5:248103:0 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Thomas, Trevor M. (1951) Some Unusual Structures in Rhaetic Sandstones, near Cowbridge, Glamorgan. Geological Magazine, 88 (6) 404-408 doi:10.1017/s0016756800069958 |
|---|
| Plain Text | Thomas, Trevor M. (1951) Some Unusual Structures in Rhaetic Sandstones, near Cowbridge, Glamorgan. Geological Magazine, 88 (6) 404-408 doi:10.1017/s0016756800069958 |
|---|
| In | (1951, December) Geological Magazine Vol. 88 (6) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | AbstractThe best known exposures of Rhaetic strata in Glamorgan are those of the Lavernock and Penarth cliff sections, where the normal black shales—thin limestones facies are displayed. In the central and west Vale of Glamorgan, however, massive sandstones are the dominant Rhaetic formation. The construction of a housing site has revealed the presence of numerous voids or cavities in these sandstones, the origin of which is attributed to decalcification. |
|---|
These are possibly similar items as determined by title/reference text matching only.
