Grampian orogeny

The Grampian orogeny was an orogeny mountain building event which affected Scotland in the middle of the Ordovician. At the time, Scotland was part of proto-North American continent Laurentia.

The orogeny overlapped with the Caledonian orogeny and the orogenies that formed the Appalachian Mountains. It was the only orogeny in Laurenta at that time which resulted in deformation, folding and metamorphism. The Fleur de Lys rocks in Newfoundland may have been affected by the Grampian orogeny as well.[1]

Sequence of the Grampian orogeny

In the Cambrian and early Ordovician, shallow water carbonates and deep water turbidite basins, which formed the Southern Highland Group, dominated the section of the Laurentian coast that would be later separate to form Scotland. The Grampian orogeny stopped sedimentation. The discovery of volcanic arc rocks in western Ireland indicated a possible island arc collision with a subduction zone during the closure of the Iapetus Ocean to form Pangea. Some proposals in 1983 and 1984 suggested that the arc is buried under younger sediments in Scotland's Midland Valley.

During the collision at the edge of the Laurentian continent, an ophiolite nappe was overthrusted, possibly preserved in Unst, in the Shetland Islands. Other ophiolite zones at the Highland Border and Ballantrae may be from the same event.

The Grampian orogeny took place at close to the same time as the Taconic orogeny. In both cases, more extensive ophiolite nappes may have eroded away.

The Grampian orogeny deformed the rocks of the Grampian Terrane and the Dalradian Supergroup. Fold traces extend for hundreds of kilometers, with a complex formation of nappes and fold stacks.[2]

References
  1. Schenk, P.E. editor (2012). Regional Trends in the Geology of the Appalachian-Caledonian-Hercynian-Mauritanide Orogen. D. Reidel Publishing Company. p. 93.
  2. Strachan, R.A. (2002). Northern and Grampian Highlands (The Geology of Scotland). The Geological Society. p. 104-107.
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