http://researchonline.federation.edu.au/vital/access/manager/Index ${session.getAttribute("locale")} 5 Grade control geological mapping in underground gold vein operations http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:4840 Wed 07 Apr 2021 13:44:23 AEST ]]> Gold mineralisation and ore controls at the Clogau mine, Dolgellau, north Wales, United Kingdom http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:4839 Wed 07 Apr 2021 13:44:23 AEST ]]> Approaches to reporting grade uncertainty in high nugget gold veins http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:4838 Wed 07 Apr 2021 13:44:23 AEST ]]> Design of grade control sampling programs for underground gold mines http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:4767 Wed 07 Apr 2021 13:44:18 AEST ]]> Grab sampling for underground gold mine grade control http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:3680 Wed 07 Apr 2021 13:34:41 AEST ]]> Asymmetrical filling of inclined crustified hydrothermal gold veins : An example from Hadleigh Castle Mine, North Queensland http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:3618 Wed 07 Apr 2021 13:34:37 AEST ]]> The importance of correct sampling and assaying practices : Case studies from gold projects http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:3593 Wed 07 Apr 2021 13:34:35 AEST ]]> Sampling - A critical component to gold mining project evaluation http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:3592 Wed 07 Apr 2021 13:34:35 AEST ]]> Continuous carbonatitic melt-fluid evolution of a REE mineralization system : Evidence from inclusions in the Maoniuping REE Deposit, Western Sichuan, China http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:2298 350 MPa) and high-density supercritical orthomagmatic fluids, characterized by SO4-rich and multicomponent composition (e.g. K, Na, Ca, Ba, Sr and REE). The dominant anion is not Cl. but SO4. The evolution of the ore-forming fluid is from a melt-fluid at high temperature, through a CO2-rich fluid at high to medium temperature to aqueous-rich fluid at low temperature. REE precipitation occurred from a high to medium temperature CO2-rich fluid. The main mechanism for REE precipitation was phase separation of CO2 and aqueous fluids resulting in a decrease of temperature and pressure. (C) 2008 Elsevier B.V. All rights reserved.]]> Wed 07 Apr 2021 13:33:21 AEST ]]> Characterisation of in situ gold particle size and distribution for sampling protocol optimisation http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:1698 Wed 07 Apr 2021 13:32:47 AEST ]]> Bulk sampling of complex gold deposits - material characterisation and program design and management http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:1697 Wed 07 Apr 2021 13:32:47 AEST ]]> Gold particle clustering : A new consideration in sampling applications http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:249 Wed 07 Apr 2021 13:31:07 AEST ]]>