Murchison Minerals Ltd. ­announced the completion of a previously reported electromagnetic and magnetic geophysical program conducted on the Brabant-McKenzie high-grade zinc deposit located near the community of Brabant Lake, Saskatchewan. The Deposit is described as a high-grade sphalerite-chalcopyrite- pyrrhotite rich volcanogenic massive sulfide occurrence which hosts a NI 43-101 indicated resource of 1.6 million tonnes grading 9.2% zinc and an inferred resource of 3 million tones grading 5.5% zinc (MPH Consulting Limited and P&E Consultants Inc. The Program was designed to confirm and define known conductors with coincident magnetic anomalies situated immediately south, along strike and to depth of the Deposit. This was the first of a number of planned ground geophysical programs designed to test numerous anomalies identified along the 15 kilometre strike of the property.

Modeled results from the Program reveal a higher conductive plate within the northern portion of a larger conductive horizon described below. This plate continues into and is coincident with mineralization associated with the Deposit along strike and extends to depth below historically intersected mineralization. The plate measures 350 metres in strike with a depth extent of over 500 metres and a 54 degree dip to the northwest.

As reported in the Technical Report, this portion of the Deposit has seen limited historic drilling with reported intersections of up to 13.3% Zn over 1.8 m in Hole 38 and 15.4% Zn over 1.5 m in Hole 40. Past drilling reveals that the Deposit has been drilled to a depth of over 700 metres down-dip, and remains open down-dip and along strike to the south. These results confirm that this area remains a priority drill target with potential to add tonnage to the Deposit.

Modeling of the data from this survey also reveals an open ended, 1.3 kilometre long conductive and magnetic horizon extending south from the Deposit with a depth extent of over 1 kilometre and a dip of approximately 50 degrees to the northwest. The direction, length, dip and depth of the modeled data are consistent with the known airborne conductor extent and historical drill results. Historical drilling along the 2015 TDEM conductor south of the Deposit area consisted of several short, near surface holes which do not appear to have adequately tested the horizon of the newly modeled conductor.

The Program consisted of a fixed loop Time Domain Electromagnetic ('TDEM') and magnetic ground survey which was conducted over 200 metres of the southern portion of the Deposit and a further 600 metres along strike to the south along 100 meter spaced lines. One line of EM surveying was conducted using a SQUID sensor for comparative purposes and confirms the higher conductive zone identified in the northern part of the survey area. The geophysical data obtained during the 2015 program will aid the Company with drill programs going forward, designed to increase the resource of the known Deposit.

The data will also be utilized in regional programs as exploration vectors to rank the numerous airborne electromagnetic and magnetic anomalies that occur within similar host rock lithologies along the 15 kilometre strike length of the Brabant property.