Abstract The Iapetus Ocean was the first ancient ocean to be identified following the
development of plate tectonics; its history has been fundamental in relating orogenesis and …

This study provides an up-to-date and comprehensive review of the Early Palaeozoic
evolution of the Brabant Massif belonging to the Anglo-Brabant Deformation Belt. Situated at …

Detailed global plate motion models that provide a continuous description of plate
boundaries through time are an effective tool for exploring processes both at and below the …

ABSTRACT The Canadian Appalachians are a segment of the long and narrow
Appalachian–Caledonian mountain belt, one of the Earth's classic orogens. The Canadian …

Major late Paleozoic faults, many with documented strike‐slip motion, have dissected the
Ordovician‐Devonian Appalachian orogen in the Maritime Provinces of Atlantic Canada …

The eastern edge of the Appalachian orogen is composed of a collection of Neoproterozoic–
early Paleozoic domains, Avalonia, Carolinia, Ganderia, Meguma, and Suwannee, which …

The supercontinent Pangea formed by the subduction of the Iapetus and Rheic oceans
between Gondwana, Laurentia, and Baltica during mid-to-late Paleozoic times. However …

The deformed margin of the Laurentian craton, preserved within the Appalachian-
Caledonide Orogen, is one of Earth's best studied ancient continental margins. Within the …

The Minas Fault Zone (MFZ) defines the boundary between the Avalon and Meguma
terranes in the Canadian Appalachians and is exposed in mainland Nova Scotia and …

The internal architecture and external form of fluvial channel bodies is governed by both
intrinsic and extrinsic controls. Extrinsic controls such as climate, eustasy, and tectonism are …