Reply to the discussion of the reply by R.L. Romer and U. Kroner on 'Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf' 1Appears in the Canadian Journal of Earth Sciences, 49(11): 1372–1377 [doi:10.1139/e2012-049]

Autor:	Uwe Kroner, Rolf L. Romer
Rok vydání:	2012
Předmět:	Paleontology Tectonics Dome Romer Geochemistry Ordovician General Earth and Planetary Sciences Sedimentary rock Geology
Zdroj:	Canadian Journal of Earth Sciences. 49:1378-1383
ISSN:	1480-3313 0008-4077
DOI:	10.1139/cjes-2012-0142
Popis:	Romer and Kroner (2012) stated “the core of the Harlech Dome (i) in part is made up of Ordovician deposits and (ii) contains tectonic repetitions”. In their comment, Schofield et al. (this issue) distort this statement and state that (i) we claim the entire sedimentary sequence of the Harlech Dome is Ordovician and (ii) we misinterpreted their zircon data. We disagree. In our reply, we demonstrate that the argumentation of Schofield et al. (this issue) is driven by circular argumentation and that their use and interpretation of U–Pb zircon data is inadequate.
Databáze:	OpenAIRE
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