Geologic Setting Sample Clauses

Geologic Setting. The Gxxxxxxx deposits are sediment hosted, micron-gold deposits whose grade is influenced by the convergence of favorable stratigraphy - often carbonaceous mudstone and silty shales, or carbonate debris flow sequences - and both high- and low-angle structures of varying orientations. The usual formations mineralized are the Cambrian Pxxxxx, Ordovician Comus, and Ordovician Valmy. The Pxxxxx is part of the eastern platform sequence, and overlain by Cambro-Ordovician platform rocks, which include Comus carbonates. Further west, the Ordovician Comus includes both calcareous and argillaceous sediments, and interbedded mafic volcanics and tuffs. Still further west, the Ordovician Valmy(?) is represented by a more siliceous, cherty or volcanic assemblage, which is usually interpreted to be in east-directed overthrust contact with Comus beneath it. Locally, a depositional contact between Comus and Valmy is sometimes inferred. The lower Paleozoic section is usually in unconformable or high-angle fault contact with overlying Pennsylvania-Permian Exxxxxx limestone, and the entire area was covered at one time by unconformable sheets of Miocene volcanics, now only preserved in isolated pockets. Unraveling the true geologic relationships is significantly complicated by the overprinting effects of 4 discrete structural events: · The Devono-Mississippian Antler orogeny, which thrust western-facies siliceous rocks over eastern-facies carbonates; · The Permo-Triassic Sonoma orogeny which reactivated thrusting · The Jurassic-Cretaceous Sxxxxx Orogeny resulting from Pacific Plate collision North American plate; · The mid-Tertiary inception of regional extensional faulting.
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Related to Geologic Setting

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