Generation Mining Ltd T.GENM

2014 Chono:

[my69z]

2014 Chonolith definition:
The largest Ni-Cu deposits are associated with an unusual and somewhat unique intrusion termed a chonolith. A chonolith is an irregular to pipe like intrusion. The intrusion geometry defines the outer footprint of the Ni-Cu sulfide deposit. The deposit itself is hosted within and often fills or is centrally located within the intrusion i.e. not restricted to the basal contact. A key feature is that the massive sulfides are often discordant with respect to disseminated sulfides and are hosted in a distinctive variably textured facies.

May 25, 2021 Generation:
The Chonolith Zone is an irregular-to-pipe-like shaped intrusive body which may have been a conduit through which magma responsible for the Marathon Deposit flowed. Much of the previous drilling (early 2000s) in this area was quite shallow; however, some deeper holes, notably BO-06-20 which assayed 0.93 g/t Pd, 0.25 g/t Pt, 0.10 g/t Au and 0.58% Cu over a 100.5 metre interval (from 215.8 m to 316.3 m downhole), returned elevated Pd and Cu assays. Given the nature and geometry of the intrusion, which may have constrained and focused magma flow, there is the potential for massive sulphide accumulation along the floor of the Chonolith as well as disseminated Cu and Pd mineralization throughout the intrusive itself.

It's been 15 years since our Chono was followed up. 
They clearly understand what they are & of course used new technology on our's.
Glta!!

The chonolith Ni-Cu model: expanding the footprint of Ni-Cu deposits and chasing weaknesses in the Nickel mineral system model (segweb.org)