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Hierro-Cobre Cobre-Oro

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Corte con serie de<br />

diques ultramáficos<br />

WPT<br />

Sample<br />

Composition<br />

Additional description<br />

Orient.<br />

Width<br />

Iron oxides<br />

Other<br />

241<br />

L-740<br />

Peral. Na Fe<br />

trachy phonolite<br />

Very fine-grained, glassy, gray-reddish to dk pk-bn; no<br />

reaction to HCl. Conchoidal fracture and sharp edges.<br />

056°90°<br />

1 m<br />

w/ diss fine<br />

magnetite<br />

242<br />

L-741<br />

Meta. K Fe trachy<br />

phonolite<br />

Magnetic, dark gray to bk , subvolcanic. With extremely finegrained<br />

matrix, plagiolase porphyries, open vacuoles; does not<br />

react to HCl; chloritization. Nepheline blades 2-3mm wide,<br />

range to 2cm long.<br />

078°90°<br />

243<br />

Carbonatite<br />

Bk to dk bn with hematitic banding along foliation, coarse<br />

hematite clusters and gossanous texture.<br />

60°/78°<br />

S<br />

Very abun-dant<br />

FeOx<br />

244<br />

L-742<br />

Metal.Na Mg<br />

biotite granite<br />

Very fine-grained, medium gray, foliated, with slightly<br />

magnetic character.<br />

245<br />

L-743<br />

Carbonatite<br />

Brown, very magnetic, with internal flow banding.<br />

085/52°<br />

S<br />

1m<br />

abundant earthy<br />

goethite after<br />

sulfides<br />

246<br />

L-745<br />

Carbonatite<br />

Strongly magnetic, very fine-grained, medium gray; internal<br />

flow banding; intersects L-742. Alteration halo around dike;<br />

sample has 2 “quenched” margins.<br />

095/49°<br />

S<br />

4-5 cm<br />

none visible<br />

247<br />

L-746<br />

Carbonatite<br />

Weathering surfaces show clusters of Fe oxide-rich substance<br />

that does not weather as much. Surface is bn/yw with very<br />

irregular texture like lapiez corrosion in karstic environments.<br />

064/83°<br />

S<br />

Abundant bk.<br />

Braided magnetite<br />

bodies,<br />

contain sulfs<br />

Min.<br />

length<br />

=<br />

400m<br />

251<br />

Carbonatite<br />

With abundant iron oxide alteration and red-rock alteration in<br />

the host rocks.<br />

Subvert<br />

ical<br />

25-<br />

30cm<br />

252<br />

L-747<br />

Quartz vein<br />

With red Feox stains, thin red- and bk-filled joints<br />

050/90°<br />

10-<br />

15cm

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