Gold Price (USD) 1271.11
TSX.V NVO
OTCQX NSRPF

Comet Well

Novo acquired an 80% interest in the Comet Well project in 2017. Comet Well is a significant new conglomerate-hosted gold discovery situated approximately 45 km south of Karratha, Western Australia. Prospectors first discovered gold nuggets here around mid-2016 and have remained very active in the area since. Novo confirmed the origin of gold is from a package of previously unmapped conglomerates at the base of the Archean Fortescue Group, the same unit that hosts Novo’s Beatons Creek project approximately 350 km east.

Map showing Novo’s 100% controlled mineral holdings, Novo-Artemis farm-in/joint venture holdings and Comet Well consolidated holdings in the Karratha region.
Map showing Novo’s 100% controlled mineral holdings, Novo-Artemis farm-in/joint venture holdings and Comet Well consolidated holdings in the Karratha region.)

Map showing Novo’s mineral holdings in the Comet Well-Purdy’s Reward area.
Map showing Novo’s mineral holdings in the Comet Well-Purdy’s Reward area.

At Comet well, detectorists have been active over an 8 km corridor underlain by conglomerates. Recently, gold has been discovered in situ in several locations. Gold nuggets in the matrix of conglomerates are typically coarse, +2 mm, and distinctly flattened appearing like watermelon seeds. Gold purity is high, 96-98%, setting it apart from gold derived from orogenic lode deposits in the underlying basement that displays purities of 70-95%.

(Photograph of the Comet Well area looking south. Weathered, gold-bearing conglomerates occupy the foreground. Note liberated quartz cobbles scattered across the surface. Mt. Roe basalt underlies the hills in the middle ground and the Cooya Pooya dolerite sill forms the ridge in the back. These rocks comprise the base of the Fortescue Group in this area and dip shallowly, less than 5 degrees, to the south. Novo-Artemis farm-in/joint venture ground covers the foreground. Novo’s 100% controlled ground lies in the distance and further into the basin.)

(Examples of in situ gold nuggets frozen in matrix material from the Comet Well and Purdy’s Reward area. Rock is dark grey-green to brown hornfelsed sandy conglomerate. Gold is high purity, 96-98%, setting it apart from that from basement-hosted lode gold deposits which commonly displays purities of 70-95%. Note that nuggets are rounded, clear evidence they are detrital in origin. Multiple outcrops of gold-bearing conglomerate have recently been identified at Comet Well and Purdy’s Reward. Novo plans to assess such areas first during upcoming exploration activities.)

(Liberated “watermelon seed” type gold nugget from the Comet Well area. Blue lines are 1 mm apart. Note the dimpled surface, a result of imprinting of sandy matrix on the nugget during compaction after burial. Otherwise, the original shape of the nugget is well-preserved.)

(Cross sectional view of a “watermelon seed” style gold nugget in a sawn slab of gold-bearing conglomerate. The dark grey-green color is likely a product of thermal metamorphism, hornfels, of the original rock. Note the crenulated texture around the edge of the nugget. Encircling the nugget is a cloud of very fine gold, likely remobilized during burial or metamorphism. Such dispersed gold is common around in situ nuggets at Comet Well and Purdy’s Reward.)

Sign-Up

Sign up to receive latest news and recent projects from NOVO Resources