| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Note on the Tectonic Style of the Ord Ban Quartzites, Mid-Strathspey |
|---|
| Journal | Geological Magazine |
|---|
| Authors | McIntyre, Donald B. | Author |
|---|
| Year | 1951 (February) | Volume | 88 |
|---|
| Issue | 1 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800068916 |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 248010 | Long-form Identifier | mindat:1:5:248010:1 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | McIntyre, Donald B. (1951) Note on the Tectonic Style of the Ord Ban Quartzites, Mid-Strathspey. Geological Magazine, 88 (1) 50-54 doi:10.1017/s0016756800068916 |
|---|
| Plain Text | McIntyre, Donald B. (1951) Note on the Tectonic Style of the Ord Ban Quartzites, Mid-Strathspey. Geological Magazine, 88 (1) 50-54 doi:10.1017/s0016756800068916 |
|---|
| In | (1951, February) Geological Magazine Vol. 88 (1) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | AbstractStudy of profiles, perpendicular to the fold-axes, shows that the folding is disharmonic. Nearly every s−surface is one of décollement. In some exposures the quartzites are reduplicated by superposed recumbent-folds without infolds of other material. The contacts are tectonic and not stratigraphic. Incipient boudinage is frequent, and nearly all surfaces show well-developed b−lineation. |
|---|
These are possibly similar items as determined by title/reference text matching only.
