| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | The Ordovician–Silurian boundary at the eastern end of Anticosti Island |
|---|
| Journal | Canadian Journal of Earth Sciences |
|---|
| Authors | Cocks, L. R. M. | Author |
|---|
| Copper, P. | Author |
| Year | 1981 (June 1) | Volume | 18 |
|---|
| Issue | 6 |
|---|
| Publisher | Canadian Science Publishing |
|---|
| DOI | doi:10.1139/e81-099Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 477132 | Long-form Identifier | mindat:1:5:477132:0 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Cocks, L. R. M., Copper, P. (1981) The Ordovician–Silurian boundary at the eastern end of Anticosti Island. Canadian Journal of Earth Sciences, 18 (6) 1029-1034 doi:10.1139/e81-099 |
|---|
| Plain Text | Cocks, L. R. M., Copper, P. (1981) The Ordovician–Silurian boundary at the eastern end of Anticosti Island. Canadian Journal of Earth Sciences, 18 (6) 1029-1034 doi:10.1139/e81-099 |
|---|
| In | (1981, June) Canadian Journal of Earth Sciences Vol. 18 (6) Canadian Science Publishing |
|---|
| Abstract/Notes | A Hirnantia fauna is recorded for the first time from Anticosti Island, situated 6 m below the beds interpreted here as representing the maximum regression at the eastern end of the island, the latter coinciding with the local top of the revised Ellis Bay Formation. The Ordovician–Silurian boundary on the island is discussed. |
|---|
These are possibly similar items as determined by title/reference text matching only.
