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Western Yilgarn Spots Five New Gold Targets at Ida Holmes Junction

Mining By Maxwell Dee 3 min read

Western Yilgarn NL has identified five promising gold exploration targets at its Ida Holmes Junction Project, revealing a thick concealed greenstone belt and structural links to major gold systems in Western Australia.

  • First systematic gold evaluation at Ida Holmes Junction
  • 1,000m-thick concealed greenstone belt uncovered
  • Five high-priority targets span orogenic, hydrothermal, and palaeochannel styles
  • Previous shallow drilling missed fresh bedrock beneath alluvial cover
  • Planned aircore drilling and mapping to test targets soon

Hidden Greenstone Belt Reveals New Gold Potential

Western Yilgarn NL (ASX:WYX) has unveiled a significant new chapter for its Ida Holmes Junction Project in Western Australia, marking the first dedicated gold exploration in an area historically focused on uranium and nickel. The company’s prospectivity review has confirmed a previously unknown greenstone belt up to 1,000 metres thick buried beneath alluvial cover, intersecting the crustal-scale Ida Fault. This fault connects northwards to the Waroonga Shear Zone, a structural corridor hosting multi-million-ounce gold deposits like Agnew and Bellevue.

Structural Footprint Aligns with Major Gold Systems

The newly identified greenstone sequence lies within a major structural framework that Western Yilgarn believes is highly prospective for orogenic gold mineralisation. Recent field reconnaissance found classic hydrothermal indicators including quartz veins and cobalt-bearing asbolane minerals along key faults such as the Waroonga Shear Zone and Ballard Fault. These features are consistent with fluid pathways known to concentrate gold in the Eastern Goldfields region.

Shallow Drilling Previously Missed Bedrock Targets

Historical and recent drilling programs have largely failed to test the fresh bedrock due to an extensive transported alluvial cover averaging 5 to 8 metres thick. Western Yilgarn’s 2023 auger drilling was limited to about 2 metres depth, sampling only transported granitic alluvium rather than the underlying greenstone. This explains why earlier programs did not detect any gold anomalies, highlighting the need for deeper drilling to unlock the project’s true potential.

Five High-Priority Gold Targets Defined

Western Yilgarn has delineated five compelling targets spanning three gold styles: a thick under-explored greenstone belt analogous to Agnew and Bellevue mines; overlying palaeochannel systems prospective for alluvial gold derived from weathered bedrock; hydrothermal intrusive zones marked by brecciated quartz veins and cobalt-rich minerals; shear-hosted lodes along the Waroonga Shear Zone with ferruginous quartz veins; and regional palaeochannels capable of hosting placer gold deposits. This multi-pronged approach aims to maximise discovery chances across both bedrock and cover sequences.

Drilling and Mapping to Follow Regulatory Approvals

The company’s immediate focus is to secure regulatory approvals and mobilise drilling contractors to commence aircore drilling designed to penetrate the transported cover and sample fresh bedrock. Complementary rock chip sampling and detailed geological mapping will target outcropping zones along the major shear and fault structures. The integration of these results with existing geophysical data will refine targets for potential follow-up reverse circulation or diamond drilling programs.

Western Yilgarn’s Chairman Peter Michael emphasised the significance of this discovery, noting the technical robustness of the exploration strategy and the exciting opportunity to test a previously concealed gold system in one of Western Australia’s most prospective regions.

Bottom Line?

Western Yilgarn’s unveiling of thick concealed greenstone and structurally controlled gold targets at Ida Holmes Junction sets the stage for a pivotal exploration phase, with drilling results poised to clarify the project’s true gold potential.

Questions in the middle?

  • Will aircore drilling beneath transported cover confirm bedrock gold mineralisation?
  • How might the identified hydrothermal indicators correlate with gold grades once sampled?
  • Could the palaeochannel systems host economically viable alluvial gold deposits?