PALEOZOIC ARC AND DEFORMATION ZONE DISTRIBUTION AROUND EASTERN AVALONIA AND ITS TECTONIC SIGNIFICANCE
Concealed beneath younger rock in Eastern England, but recorded in several borehole sections, the continuation of the Lake District magmatic arc curves southeast and extends as the Anglo-Brabant Deformation Belt (ABDB) to the Brabant Massif in Belgium. East of the ABDB the southern North Sea - Luneberg Terrane (SNSLT) is also thought to be part of Avalonia because basement is exposed as end-Proterozoic ("Panafrican") granite gneisses in inliers from NW Germany, and borehole faunal and sediment provenance evidence from Rugen indicates the arrival of Panafrican age detritus, with Gondwana-related fossils in the Ashgill, coeval with convergence of established Avalonian crust with Laurentia and Baltica. The transpressional Heligoland-Pomerania Deformation Belt, marking the contact of the SNSLT with Baltica lacks significant magmatism.
Finally, Siluro-Devonian sporadic calc-alkaline magmatism along the "southern" Avalonian margin of Laurussia developed above a subducting Rheic Ocean plate.