Romer, Rolf L., Kroner, Uwe (2012) Reply to the discussion by J.W.F. Waldron and C.E. White on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf”1Appears in Canadian Journal of Earth Sciences, 2012, 49(6): 772–774 [doi: 10.1139/e2012-004]. Canadian Journal of Earth Sciences, 49 (6) 775-780 doi:10.1139/e2012-006
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Reply to the discussion by J.W.F. Waldron and C.E. White on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf”1Appears in Canadian Journal of Earth Sciences, 2012, 49(6): 772–774 [doi: 10.1139/e2012-004]. | ||
| Journal | Canadian Journal of Earth Sciences | ||
| Authors | Romer, Rolf L. | Author | |
| Kroner, Uwe | Author | ||
| Year | 2012 (June) | Volume | 49 |
| Issue | 6 | ||
| Publisher | Canadian Science Publishing | ||
| DOI | doi:10.1139/e2012-006Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 484831 | Long-form Identifier | mindat:1:5:484831:2 |
| GUID | 0 | ||
| Full Reference | Romer, Rolf L., Kroner, Uwe (2012) Reply to the discussion by J.W.F. Waldron and C.E. White on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf”1Appears in Canadian Journal of Earth Sciences, 2012, 49(6): 772–774 [doi: 10.1139/e2012-004]. Canadian Journal of Earth Sciences, 49 (6) 775-780 doi:10.1139/e2012-006 | ||
| Plain Text | Romer, Rolf L., Kroner, Uwe (2012) Reply to the discussion by J.W.F. Waldron and C.E. White on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf”1Appears in Canadian Journal of Earth Sciences, 2012, 49(6): 772–774 [doi: 10.1139/e2012-004]. Canadian Journal of Earth Sciences, 49 (6) 775-780 doi:10.1139/e2012-006 | ||
| In | (2012, June) Canadian Journal of Earth Sciences Vol. 49 (6) Canadian Science Publishing | ||
| Abstract/Notes | In their comment, Waldron and White state that manganese-rich sedimentary rocks of Nova Scotia and Wales are Cambrian and were deposited in a deep-water turbidite basin called “Megumia” rather than on the Avalonian shelf. Available geochronological data are not in conflict with an Early Ordovician deposition age for manganese-rich sedimentary rocks north of the Rheic suture, including those of Nova Scotia and northern Wales. “Megumia” is part of the Avalonian plate, and the manganese-rich sediments were deposited on its shelf. | ||
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