Predictive Mineralogy

Possible unrecorded species at Remetské Hámre, Sobrance District, Košice Region, Slovakia

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing species	Formula	Match %	Due to recorded presence of
Gold	Au	70.64%	Benjaminite (58.82 %), Tetradymite (71.62 %)
Zircon	Zr(SiO₄)	64.45%	Monazite-(Ce) (54.99 %), Xenotime-(Y) (56.84 %)
Cassiterite	SnO₂	61.83%	Stannite (61.84 %)
Pyrophyllite	Al₂Si₄O₁₀(OH)₂	57.54%	Zunyite (57.55 %)
Alunite	KAl₃(SO₄)₂(OH)₆	52.83%	Zunyite (52.83 %)
Silver	Ag	50.31%	Acanthite (50.32 %)
Chalcocite	Cu₂S	50.30%	Covellite (50.30 %)

Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)

Predicting paragenetic modes of deposit

Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.

Paragenetic Mode	Score
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) Unique: Benjaminite, Boulangerite, Bournonite	296
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] Unique: Halloysite	100
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)	41
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)	32
48 : Soil leaching zone minerals	24
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)	22
31 : Thermally altered carbonate, phosphate, and iron formations	21
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)	17
49 : Oxic cellular biomineralization (see also #44)	12
26 : Hadean detrital minerals	10
34 : Complex granite pegmatites	9
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]	8