Cargill Township carbonatite complex, District of ... - Geology Ontario
Cargill Township carbonatite complex, District of ... - Geology Ontario
Cargill Township carbonatite complex, District of ... - Geology Ontario
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R. P. SAGE<br />
with brown cores and reddish brown rims; grains display weak bending <strong>of</strong> (001) cleavage and<br />
wavy extinction. Apatite forms rounded anhedral grains some <strong>of</strong> which are elongate. Carbonate<br />
forms anhedral irregular grains with curved to lobate grain boundaries.<br />
Reference No. 798<br />
Sample No. CCM24 333.4-333.7<br />
Clinohumite, amphibole, phlogopite, apatite, magnetite sovite.<br />
Fine to medium grained, massive, inequigranular-seriate, allotriomorphic, with curved grain<br />
boundaries. Clinohumite forms anhedral yellowish grains, possibly after olivine. Clinohumite<br />
contains acicular amphibole. Magnetite is anhedral in form and disseminated throughout.<br />
Apatite forms anhedral rounded to elongate grains. Phlogopite forms anhedral irregular grains<br />
with pale brown cores and reddish brown rims. Amphibole forms euhedral acicular crystals,<br />
some <strong>of</strong> which are twinned. Carbonate forms anhedral interlocking mosaic <strong>of</strong> grains with curved<br />
grain boundaries.<br />
\<br />
Reference No. 799<br />
Sample No. CCM24 346.5-346.9<br />
Phlogopite, apatite sovite.<br />
Fine grained, inequigranular-seriate, allotriomorphic, with curved to straight grain boundaries.<br />
Apatite forms rounded anhedral grains; some are elongate in outline. Phlogopite forms an<br />
hedral, brown to reddish brown grains. Carbonate forms an interlocking mosaic <strong>of</strong> anhedral<br />
grains with straight to curved grain boundaries.<br />
Reference No. 800<br />
Sample No. CCM24 357.4-357.75<br />
Olivine, amphibole, apatite, magnetite sovite.<br />
Fine to medium grained, inequigranular-seriate, allotriomorphic, with curved to lobate grain<br />
boundaries. Olivine is both fresh and extensively altered to clinohumite. Amphibole forms<br />
euhedral pale green to colourless acicular crystals and is closely associated with olivine. Apatite<br />
forms rounded anhedral grains some <strong>of</strong> which are elongated in outline. Magnetite forms an<br />
hedral disseminated grains. Carbonate forms an interlocking mosaic <strong>of</strong> anhedral grains with<br />
curved to lobate grain boundaries.<br />
Reference No. 801<br />
Sample No. CCM26 68.6-68.9<br />
Pyrrhotite, magnetite, clinohumite, phlogopite, apatite sovite.<br />
Fine to medium grained, massive, inequigranular-seriate hypiodmorphic. Carbonate forms an<br />
interlocking mosaic <strong>of</strong> anhedral grains. Apatite forms rounded <strong>of</strong>ten elongate grains.<br />
Clinohumite forms minor anhedral grains, commonly in association with altered olivine or re<br />
placing olivine. Phlogopite forms anhedral pleochroic reddish brown grains, rarely with poikilitic<br />
apatite. Magnetite forms anhedral irregular disseminated grains. Pyrrhotite forms anhedral, ir<br />
regular, disseminated grains. Trace to minor amounts <strong>of</strong> serpentinized olivine, and amphibole<br />
are present.<br />
Reference No. 802<br />
Sample No. CCM26 86.25-86.65<br />
Olivine, apatite, phlogopite, magnetite sovite.<br />
Fine to medium grained, massive, inequigranular-seriate, massive, hypidiomorphic. Apatite<br />
forms anhedral to subhedral rounded to rounded-elongate grains. Magnetite forms anhedral<br />
irregular disseminated grains. Olivine forms rounded to elongate grains with local alteration to<br />
clinohumite. Phlogopite forms pleochroic, anhedral to subhedral grains <strong>of</strong> pale reddish brown<br />
colour. Carbonate forms an interlocking mosaic <strong>of</strong> grains.<br />
Reference No. 803<br />
Sample No. CCM26 89.25-89.6<br />
Olivine, phlogopite, apatite, magnetite sovite.<br />
Fine to coarse grained, massive, inequigranular-seriate, hypidiomorphic. Apatite forms<br />
rounded sometimes elongate crystals which are subhedral in form. Olivine forms anhedral<br />
somewhat elongated grains with local alteration to clinohumite and serpentine. Magnetite forms<br />
anhedral irregular disseminated grains. Phlogopite forms anhedral to subhedral pale brown<br />
pleochroic grains. Carbonate forms an interlocking anhedral mosaic <strong>of</strong> grains.<br />
Reference No. 804<br />
Sample No. CCM26 101.65-102.0<br />
Olivine, phlogopite, magnetite, apatite sovite.<br />
Fine to medium grained, massive, inequigranular-seriate, hypidiomorphic. Apatite forms an<br />
hedral to subhedral grains, some <strong>of</strong> which are elongate in outline. Phlogopite forms pale brown<br />
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