Laxfordian orogeny

id: laxfordian-orogeny-291-7981983
title: Laxfordian orogeny
text: The Laxfordian orogeny was an orogenic event between 1.9 and 1 billion years ago. It primarily affected the North Atlantic Craton, in particular a section that cleaved off during the Mesozoic as the Scottish Shield Fragment, part of the Lewisian complex within the Hebridean Terrane. The event produced deformation and high-grade metamorphism, migmatite formation and the emplacement granite and pegmatite in the Loch Maree Group basement rocks between 1.9 and 1.8 billion years ago. From 1.6 to 1.4
brand slug: wiki
category slug: encyclopedia
description: Geologic event
original url: https://en.wikipedia.org/wiki/Laxfordian_orogeny
date created:
date modified: 2023-03-06T22:14:34Z
main entity: {"identifier":"Q97328175","url":"https://www.wikidata.org/entity/Q97328175"}
image:
fields total: 13
integrity: 14

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