As you can see from the scale that bar that I have ringed on the...

As you can see from the scale that bar that I have ringed on the Tetris magnetic image below, the Tetris point magnetic anomaly is well over a Kilometre wide.

Most of the drilled metres of the angled drill hole were used to get down through the 450m of cover (so maybe the top 520m of the hole?), and as Antipa says, the tail of the hole only succeeded in traversing 150m horizontal width of the 1,200m wide Tetris magnetic feature.

The hole did not satisfactorily explain the intense point magnetic anomaly, because no magnetic mafic igneous rocks were intersected and nor was there anywhere near enough sulphide or any magnetite to explain it.

However, the short basement section of the hole did intersect quartz veins up to 3m wide, which is pretty encouraging in my book, along with significant widths (up to 20m) of hydrothermal alteration and what sound like interesting amounts of sulphides, including pyrite veinlets.

So overall, I would say this is a successful first test of Tetris: they got through the cover without any major problems, hit quartz-sulphide veining and hydrothermal alteration in the basement, and have yet to drill the source of the magnetic anomaly.

Sounds promising. And agree with GeoFiji: sounds like the first hole into Haveiron. Fingers crossed for gold values (I'd be cutting the core right now and paying a premium to fast track it through the lab if it was me)

Tetris lives!