SGR's information seams to mitigate the presence of WEL..... The axis is acknowledged to be Horseshoe lake, and convienintly runs as far East as san Gold 1.... But it think mitigated again as the eastern axis is likely further east in the siderock Garner area.

From the old Goldmau report:

Rocks in the Rice Lake Gold Belt are similar in age to those at Red Lake. Gold

mineralization is present in both older rocks in the northern part of the Belt and

younger rocks in the southern part of the belt. The San Antonio mine, which has

contributed over 80% of the gold production from the belt to date, is hosted in the

younger southern package of rocks.

Limited production has been obtained from deposits in the northern part of the Belt.

Nonetheless, the older rocks of the northern portion of the belt are considered highly

prospective as they are regarded as equivalent to the Balmer series of rocks that host

the world class gold mineralization at Red Lake.

Sections of the Rice Lake Belt are also cut by the Wanipigow Fault. This is a

regional shear fault that cuts through the Rice Lake Belt and extends eastwards to

the Red Lake and Pickle Lake gold camps.

Crustal breaks such as the Wanipigow Fault are often associated with the major gold

camps throughout the Canadian Shield such as the Timmins gold camp. Since 1910,

the Timmins area has produced nearly 70 million ounces of gold, making it one of

the two of most productive gold camps in North America.