Off The Dining Area Are French Doors That Lead To A Large, Freshly Stained, Multi-level Deck. The Home Offers Three Carpeted Bedrooms And The Primary Bedroom Is Located On The Back Corner. Down The Hallway, To The Left, You Will Find The Bathroom With Laminate Flooring, Updated Vanity, Lighting And Mirror. The Kitchen Features Stainless Appliances That Includes A New Refrigerator, Custom Tile Backsplash And Updated Countertops. The Kitchen And Dining Area Are Bright And Open With An Abundance Of Natural Light That Spills In From The French Doors. The Home Has Been Freshly Painted & Updated Gray Laminate Flooring That Runs Throughout The Space. As You Enter, You Are Greeted With A Living Room That Features A Vaulted Ceiling And Brick Wood-burning Fireplace. This Ranch-style Home Has Many Updated Features Located In A Quiet Cul-de-sac. Roof Was Replaced In 2019.ĭescription Of 12303 Twelveoaks Ct Midlothian, VA 23112 The Home Also Features A Detached Garage With New Roll-up Door Which Is Perfect For A Workspace. The Backyard Is Also Spacious And Fenced In. The Backyard Is Perfect For Entertaining And Offers Privacy With Views Of The Water.
This Ranch-style Home Has Many Updated Features Located In A Quie t Cul-de-sac. Mineralization is characterized by gold associated with barite, pyrite, decalcification and silicification hosted in the Webb Formation at the contact with the Devonian Guilmette limestone.Welcome To 12303 Twelveoaks Court. At nearby deposits, mineralization is strongly controlled by anticlines (Rain) and extensional faults (Emigrant Springs). Alteration appears to be structurally controlled, and may have leaked into the upper plate directly above mineralized lower-plate rocks.Īnomalous pathfinders (As, Sb) have been identified on the project area through reconnaissance rock chip sampling. The alteration is expressed as sulfidation, silicification and local decalcification in the allochthonous upper plate rocks.
The host rocks are composed of both the allochthonous calcareous mudstones and carbonate rocks of the Devonian Woodruff, Mississippian Webb, and Chainman Formations, as well as the eastern facies carbonate rocks. Syn- to post-mineral extensional faulting has acted as fluid conduits and/or cuts and offsets mineralization. Anticlinorium formed as a result of the contractional deformation. Pre-mineral compressional faulting (Roberts Mountain Thrust) have juxtaposed western facies siliciclastic rocks on top of eastern facies carbonate rocks. The Spring Canyon property position is located immediately north of the mineralized Rain structural corridor and the Mud Springs property is located northeast of the Emigrant Springs deposit. Spring Canyon and Mud Springs are Carlin-type gold projects located ~6 km southeast of Carlin, Nevada and are available for partnership.
Skellefte Gold - Akerberg & Rismyrliden.
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