Overview of Results from the Greenstone ... - Geology Ontario
Overview of Results from the Greenstone ... - Geology Ontario
Overview of Results from the Greenstone ... - Geology Ontario
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03VOI-0422-1 Trachytic lava, Timiskaming assemblage, Gauthier Township<br />
(NAD83, Zone 17 UTM 587842E, 5332221N; #31 on Figure 2 and Table 1)<br />
Sample 03VOI-0422-1 was collected <strong>from</strong> a distinct unit <strong>of</strong> feldspar-phyric trachytic lava <strong>from</strong> <strong>the</strong><br />
volcanic-dominated section <strong>of</strong> <strong>the</strong> Timiskaming assemblage in central Gauthier Township.<br />
A modest amount <strong>of</strong> zircon was recovered <strong>from</strong> this sample, dominated morphologically by small,<br />
short (2-3:1), generally cylindrical and <strong>of</strong>ten sharply terminated prisms. For <strong>the</strong> most part, zircons were<br />
colourless to brown and free <strong>of</strong> cracks and inclusions, but distinct cores were visible in some grains and<br />
were avoided where possible.<br />
Analytical data for two abraded single grains and one fraction comprising two small grains are 0.3 to<br />
3.2% discordant and yield overlapping 207 Pb/ 206 Pb ages between 2668.3 and 2670.1 Ma (Table A1). The<br />
strongly collinear nature <strong>of</strong> <strong>the</strong> data enable a regression line to be fit through <strong>the</strong> origin that provides an<br />
upper intercept age <strong>of</strong> 2669.6±1.4 Ma (71% probability <strong>of</strong> fit; MSWD = 0.34; Figure 7C). Two o<strong>the</strong>r<br />
fractions, consisting <strong>of</strong> a single, colourless stubby prism (A2) and two small short brown prisms (A4) are<br />
only slightly discordant (0.6%), but have distinctly higher 207 Pb/ 206 Pb ratios than <strong>the</strong> previous fractions.<br />
Their corresponding ages, at 2694 and 2676 Ma, respectively, suggest minor amounts <strong>of</strong> inheritance—<br />
possibly <strong>from</strong> Porcupine and even earliest Timiskaming sources—although <strong>the</strong> ages should be regarded<br />
as strictly minimum estimates.<br />
The 2669.6±1.4 Ma age for <strong>the</strong> early Timiskaming assemblage alkaline volcanic rock <strong>from</strong> Gauthier<br />
Township is younger than any previous depositional estimate based on <strong>the</strong> youngest measured detrital<br />
zircons <strong>from</strong> <strong>the</strong> Timiskaming Group in <strong>the</strong> Timmins, Kirkland Lake or Larder Lake areas (Corfu,<br />
Jackson and Sutcliffe 1991; Ayer et al. 2003). However, this age is in accord with maximum age<br />
estimates <strong>of</strong> Timiskaming assemblage sandstone and conglomerate deposition <strong>from</strong> <strong>the</strong> uppermost Three<br />
Nations formation (