Palaeoproterozoic to Mesoproterozoic Geology of North Queensland
Palaeoproterozoic to Mesoproterozoic Geology of North Queensland
Palaeoproterozoic to Mesoproterozoic Geology of North Queensland
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Other Proterozoic Inliers – Coen•Holroyd Group– Divided in<strong>to</strong> 5 named units– Fine <strong>to</strong> medium-grained clastic sediments becomingmore pelitic <strong>to</strong> east– Some mafic rocks with MORB-like geochemistry– Iso<strong>to</strong>pic constraints (OZCHRON)• Laminated slate has a MDA <strong>of</strong> 1560±22Ma with a widerange <strong>of</strong> older ages up <strong>to</strong> ~3300Ma• Phyllite has a MDA <strong>of</strong> 1550±10Ma with other agegroups at ~1593, ~1639 1696 and ~1750Ma• Zircon rims in a gneiss sample have an age <strong>of</strong>1430±10Ma•Edward River Metamorphic Group– Divided in<strong>to</strong> 5 named units– Similar siliciclastic sedimentary rocks <strong>to</strong> Holroyd Group– No iso<strong>to</strong>pic constraints•Sef<strong>to</strong>n Metamorphics– Schist, quartzite, phyllite, greens<strong>to</strong>ne, marble, calcsilicatesand irons<strong>to</strong>ne– MDA zircon age <strong>of</strong> ~1200Ma – probably Neoproterozoic <strong>to</strong>Cambrian