A trans-Iapetus transform fault control for the evolution of the Rheic Ocean: Implications for an early Paleozoic transition of accretionary tectonics: Reply

A trans-Iapetus transform fault control for the evolution of the Rheic Ocean: Implications for an early Paleozoic transition of accretionary tectonics

Diagenetic Controls on the Formation of the Anarraaq Clastic-Dominated Zn-Pb-Ag Deposit, Red Dog District, Alaska

Paleolatitude and tectonic rotations of the Early Carboniferous Fountain Lake Group, Cobequid Highlands, Nova Scotia, Canada

Meguma terrane orocline: U–Pb age and paleomagnetism of the Silurian Mavillette gabbro, Nova Scotia, Canada

The amalgamation of Pangea: Paleomagnetic and geological observations revisited

Detrital zircon characterization of early Cambrian sandstones from East Avalonia and SE Ireland: implications for terrane affinities in the peri-Gondwanan Caledonides

New insights into the Bedrock and Quaternary Geology of St. George’s Bay from a vertical integration of marine datasets, offshore western Newfoundland

How was the Iapetus Ocean infected with subduction?

Ganderia–Laurentia collision in the Caledonides of Great Britain and Ireland

Evaporite tectonics and the late Paleozoic stratigraphic development of the Cumberland basin, Appalachians of Atlantic Canada

Discussion of the reply by R.L. Romer and U. Kroner on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf” 1 Appears in Canadian Journal of Earth Sciences, 49 (6): 775–780, 10.1139/e2012-006 .

Stratigraphy of the upper Hazelton Group and the Jurassic evolution of the Stikine terrane, British Columbia 1 ESS Contribution 20120051.

Discussion of "Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf"

Laurentia-derived detritus in the Badger Group of central Newfoundland: deposition during closing of the Iapetus Ocean 1 This article is one of a series of papers published in CJES Special Issue: In honour of Ward Neale on the theme of Appalachian and Grenvillian geology. 2 Geological Survey of Canada Contribution 20110273.

Cambrian successions of the Meguma Terrane, Nova Scotia, and Harlech Dome, North Wales: dispersed fragments of a peri-Gondwanan basin?

The evolutionary significance of a Lower Cambrian trace-fossil assemblage from the Meguma terrane, Nova Scotia

Kennetcook thrust system: late Paleozoic transpression near the southern margin of the Maritimes Basin, Nova Scotia

Truncation and translation of Appalachian promontories: Mid-Paleozoic strike-slip tectonics and basin initiation

Provenance of the Meguma terrane, Nova Scotia: rifted margin of early Paleozoic Gondwana