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- W2417582570 abstract "The LeBlanc-Wellington lakes area of the eastern Zemlak Domain is dominated by upper amphibolite facies leucogranites, gneissic to migmatitic granitoids, and massive anatectic granites derived from these sources and from subordinate supracrustal rocks of the Murmac Bay Group. Coarse-grained granites of the ca. 2.3 Ga regional suite and pink leucogranite inferred elsewhere to have been emplaced at 1.9 Ga are both represented, and at least some of the remaining granitoid rocks are considered part of the ca. 3.0 Ga basement to the Murmac Bay Group. All of these rocks underwent three initial phases of deformation (D1 to D3), the last of which was responsible for the regional northeast-trending structural fabric that is thought to have formed during a ca. 1.9 Ga metamorphic event attributed to the Thelon-Taltson Orogeny. During the uplift following this thermotectonic culmination, widespread brittle-ductile mylonitization was particularly intense in the western map area. The post-1.9 Ga exhumation was followed by deposition of the siliciclastic Thluicho Lake Group which, together with the basement rocks, was subjected to two more phases of deformation (D4 and D5) under greenschist facies metamorphic conditions prior to ca. 1.82 Ga deposition and subsequent folding (D6) of the Martin Group. Cu-Pb-Ag vein mineralization occurs in late fracture zones best developed in mylonitic granitoids at or near the basal Thluicho Lake Group unconformity. East-trending ca. 1.82 Ga diabase dykes at several showings may have locally provided chemical traps for the mineralizing fluids, but are not considered the metal source." @default.
- W2417582570 created "2016-06-24" @default.
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- W2417582570 date "2003-01-01" @default.
- W2417582570 modified "2023-09-23" @default.
- W2417582570 title "Geology of the LeBlanc-Wellington Lakes Area, Eastern Zemlak Domain, Rae Province (Uranium City Project)" @default.
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