Description
DOWNLOAD AMIS CERTIFICATE (PDF)
Recommended Concentrations and Limits
(at two Standard Deviations)
Certified Concentrations
Au Pb Collection 1.50 0.13 g/t
Au 2A_MICP 1.36 0.25 g/t
Au PA 1.50 0.054 g/t
Ag 4A_MICP 2 1 ppm
Cu 4A_MICP 64 8 ppm
C Combustion/LECO 2.51 0.16 %
S Combustion/LECO 0.80 0.03 %
S 4A_MICP 0.78 0.1 %
LOI LOI 8.88 0.41 %
LOI XRF 10.00 0.37 %
SG SG 2.82 0.076 Dimensionless
Al 4A_MICP 6.23 0.57 %
Al FUS 6.31 0.28 %
Ba 4A_MICP 1061 71 ppm
Be 4A_MICP 2 0.3 ppm
Bi 4A_MICP 0.1 0.02 ppm
Ca 4A_MICP 1.89 0.13 %
Cd 4A_MICP 0.4 0.08 ppm
Ce 4A_MICP 35 7 ppm
Co 4A_MICP 28 1 ppm
Cr 4A_MICP 563 83 ppm
Cs 4A_MICP 3 0.3 ppm
Dy 4A_MICP 2 0.3 ppm
Er 4A_MICP 1 0.1 ppm
Eu 4A_MICP 0.7 0.1 ppm
Fe 4A_MICP 4.51 0.18 %
Ga 4A_MICP 16 2 ppm
Gd 4A_MICP 2 0.4 ppm
Hf 4A_MICP 3 0.6 ppm
Ho 4A_MICP 0.3 0.06 ppm
In 4A_MICP 0.04 0.01 ppm
K 4A_MICP 3.87 0.31 %
La 4A_MICP 18 3 ppm
Li 4A_MICP 17 2 ppm
Lu 4A_MICP 0.1 0.08 ppm
Mg 4A_MICP 2.48 0.10 %
Mg FUS 2.54 0.049 %
Mn 4A_MICP 955 48 ppm
Mn FUS 1033 113 ppm
Mo 4A_MICP 1 0.2 ppm
Na 4A_MICP 7099 367 ppm
Nd 4A_MICP 14 2 ppm
Ni 4A_MICP 211 11 ppm
P 4A_MICP 299 36 ppm
Pb 4A_MICP 27 6 ppm
Pr 4A_MICP 4 0.6 ppm
Rb 4A_MICP 119 9 ppm
Sb 4A_MICP 5 1 ppm
Sc 4A_MICP 11 2 ppm
Sm 4A_MICP 3 0.5 ppm
Sn 4A_MICP 2 0.3 ppm
Sr 4A_MICP 409 45 ppm
Ta 4A_MICP 0.4 0.3 ppm
Tb 4A_MICP 0.3 0.1 ppm
Te 4A_MICP 0.1 0.08 ppm
Th 4A_MICP 5 1 ppm
Tl 4A_MICP 0.5 0.06 ppm
Tm 4A_MICP 0.2 0.02 ppm
U 4A_MICP 2 0.2 ppm
V 4A_MICP 80 4 ppm
Y 4A_MICP 9 1 ppm
Yb 4A_MICP 1 0.3 ppm
Zn 4A_MICP 80 10 ppm
Zr 4A_MICP 95 26 ppm
Major Oxides
Certified Concentrations (at two Standard Deviations)
Al2O3 XRF 12.30 0.18 %
CaO XRF 2.72 0.031 %
Cr2O3 XRF 0.099 0.02 %
Fe2O3 XRF 6.60 0.18 %
K2O XRF 4.72 0.12 %
MgO XRF 4.23 0.11 %
MnO XRF 0.13 0.009 %
Na2O XRF 0.95 0.1 %
P2O5 XRF 0.069 0.004 %
SiO2 XRF 57.06 0.87 %
SO3 XRF 2.03 0.10 %
TiO2 XRF 0.48 0.03 %
Origin of Material
The material comes from a hydrothermal gold deposit in the Barberton Greenstone Belt. Greenstone belts are zones of variably metamorphosed mafic to ultramafic volcanic sequences with associate sedimentary rocks that occur within Archaean and Proterozoic cratons between granite and gneiss bodies. Greenstone belts are primarily formed of volcanic rocks, dominated by basalt, with minor sedimentary rocks inter-leaving the volcanic formations.
Approximate Mineral and Chemical Composition
The mineral assemblages of the samples are rich in greenschists and associated minerals. Greenschists is a generic name of minerals formed by regional metamorphism of mafic igneous rocks under the relatively low temperatures and pressures. The name greenstone originates from commonly having an abundance of green minerals such as chlorite/chamosite, Actinolite/ and amphiboles and sheets-like minerals such as biotite/muscovite. The common minerals associated with greenschists include quartz, orthoclase and calcite. The greenschists minerals are generally the pathfinders/ indicative of base metal sulphides and gold mineralisation.
