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| View ~SE showing Archaean Lewisian Gneisses (LG) emplaced over on the Glencoul Thrust (GT). The Cambro-Ordovician (CO) imbricates (I) occur above the Sole Thrust (ST), beneath which occur Cambrian quartzites (CQ). To the right, an unnamed thrust (TP) branches off the Glencoul Thrust and emplaces Cambrian Quarzites (Q) over Cambro-Ordovician imbricated sediments (I). |
