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Is London Basin fundamentally (by definition) capable of drifting east-west, or only north-south?
The London Basin is fundamentally capable of drifting east-west, contrary to the assumption that it only moves north-south. This conclusion is supported by its classification as an 'early' aulacogen, which indicates a weak zone susceptible to tectonic stress. The regional stress field, influenced by the African plate's northward movement and the rotation of Iberia and Western Europe, plays a significant role in this drift. The discussion dismisses the relevance of Wilson Cycle subduction zones for the near future, asserting that geological processes are too slow to impact the London Basin significantly.
PREREQUISITESGeologists, tectonic researchers, and students studying regional geology and plate tectonics will benefit from this discussion.