WebThe Highway-Reward copper-gold-silver pipes are hosted by the Cambro-Ordovician Mount Windsor Volcanics some 32 km south of Charters Towers in north Queensland, Australia. … WebAuriferous quartz sulfide veins of the Charters Towers goldfield are mainly hosted in oxidized I-type granitoids of the Ravenswood batholith. K-Ar and Ar-Ar isotope age data of …
Paleozoic terranes of eastern Australia and the drift history of ...
WebRavenswood sub-province is composed of the Palaeozoic Ravenswood Batholith, which was intruded into basement over a period of 100 million years, and comprises rocks ranging in … WebThe Ravenswood Batholith evolved during three main periods of intrusion spanning the Middle Ordovician to Early Permian. Most of the plutons of the first two intrusive periods … how can i fix my credit report
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WebRavenswood Batholith. The maximum apparent thickness of the succession is 9 km, assuming no structural repetition (Henderson, 1986; Berry et aI., 1992). Contacts between the Puddler Creek Formation and the Mount Windsor Formation are sharp and conformable (Berry et aI., 1992) or faulted. 2.2.2 MountWindsor Formation WebJul 21, 2024 · Field review of orogenic, intrusion-related gold and porphyry-related copper targets in the Ravenswood Batholith and Georgetown … WebThe Highway-Reward copper-gold-silver pipes are hosted by the Cambro-Ordovician Mount Windsor Volcanics some 32 km south of Charters Towers in north Queensland, Australia. The Mount Windsor volcanic and sedimentary sequence forms a 165 km long east-west trending volcano-sedimentary belt from Ravenswood in the east to near Pentland in the … how many people buried in arlington cemetery