Key Points
Background
TEM holds more than 1,000km2 1 of highly prospective tenure in the Yalgoo Region of Western Australia 2. TEM previously announced the presence of large-scale copper zinc anomalies at the Remorse Target based on geology, geochemistry and geophysics that it is progressing towards drilling 3, 4, 5 and that sampling of a previously incomplete block was recently completed.
Existing Prospectivity
TEM has for some time considered the Remorse Target to be a compelling exploration target due to a number of geological factors.
Previous geochemistry
The initial recognition of the Remorse Target was due to the observation of an anomaly in previously conducted wide-spaced regional surface geochemical sampling. The 4.5km anomaly exhibits high-grade (up to 635 ppm copper) samples 6 and has a remarkably coherent layering of elements (zinc, copper, nickel and rare earths) 7.
Geology
The primary mineralisation style being considered at the Remorse Target is Volcanogenic Massive Sulphides (VMS) with a typical geological environment being deep-sea sedimentary stratigraphy with intermingled mafic and felsic volcanics. The stratigraphy often exhibits iron enrichment in the form of banded iron formations and cherts. The presence of magnetite and significant banded iron geology at the Remorse Target is commonly spatially associated with VMS systems in general 8 and also a defining characteristic of the nearby Golden Grove copper-zinc deposit 9.
The Remorse Target features large-scale structures that offset the geology at surface and may serve as feeder systems, contributing to the potential mineralisation of the area. These potential feeder structures are significant as they are integral to the formation of many mineralised VMS systems 10.
Leave a Reply