| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | An Analcite-bearing Tuff in the Carboniferous Limestone of Derbyshire |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Sargent, H. C. | Author |
|---|
| Year | 1925 (October) | Volume | 62 |
|---|
| Issue | 10 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800106077 |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 280732 | Long-form Identifier | mindat:1:5:280732:8 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Sargent, H. C. (1925) An Analcite-bearing Tuff in the Carboniferous Limestone of Derbyshire. Geological Magazine, 62 (10) 462-463 doi:10.1017/s0016756800106077 |
|---|
| Plain Text | Sargent, H. C. (1925) An Analcite-bearing Tuff in the Carboniferous Limestone of Derbyshire. Geological Magazine, 62 (10) 462-463 doi:10.1017/s0016756800106077 |
|---|
| In | (1925, October) Geological Magazine Vol. 62 (10) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | In the course of a recent study of the microscopic characters of the pyroclastic rocks of Derbyshire, a colourless, isotropic mineral, with refractive index considerably lower than that of the balsam, was noted in a thin section of a tuff from Cressbrook Dale. The rock consists essentially of a mass of lapilli containing much yellowish basaltic glass, often partially devitrified, and many felspar laths, sometimes with straight extinction, in a cement partly of calcite, and partly of amorphous, opaque material, white or grey by reflected light, which is probably decomposed volcanic detritus, of the same nature as the “toadstone-clays” of Derbyshire. Vitro-clastic structure is abundant. |
|---|
These are possibly similar items as determined by title/reference text matching only.
