'Institute of Geological Sciences of the National Academy of Sciences of Ukraine'
Abstract
Several narrow, lenticular belts of black cherty mudstone
and siltstone (the Moffat Shales), alternating with thick
greywacke sequences, strike north-east to south-west
across Galloway with uniformly steep dip. In the Penkiln
Burn area, 13 km NNE of Newton Stewart, one such belt
is hornfelsed and considerably broadened near the southwest
margin of the Loch Doon granitic pluton. Base metal
anomalies in drainage and overburden are spatially
associated with the broadened section of the shale belt,
which is host to weakly disseminated and epigenetic
Pb-Zn-Cu mineralisation.
Within the Moffat Shale sequence highly siliceous
mudstone and siltstone are interbedded with chert,
greywacke and possibly thin tuffaceous horizons. The
broadening is structurally controlled, caused by the interference
of early structures with a major reciined fold
plunging to the south-east. Several phases of faulting and
minor intrusion have been recognised, and the abundance
of dykes is an unusual geological feature of the
area.
Lead is particularly enriched in drainage samples,
reaching approximately 1% in pan concentrates collected
close to a mineralised gossan-like zone. The main leadbearing
mineral identified in the anomalous concentrates,
and the in situ gossan material, is the secondary lead
phosphate plumbogummite. Overburden sampling proved
anomalous metal values extending for 2.3 km along
strike and 500 m across strike. Lead again shows the
greatest enrichment, with values ranging up to about
0.5 % , in soil close to the gossan. Zinc and copper give a
weaker response in both overburden and drainage, but
drilling showed that zinc, in the form of disseminated
sphalerite, has a greater incidence at depth than was suggested
by the surface anomalies.
Three varieties of mineralisation have been recognised.
The earliest consists of fine disseminations, chiefly of
sphalerite and pyrite, in the hornfelsed sediments. It is
characterised by zinc levels between 500 and 1000 ppm
over several metres of drill core; lead levels rarely exceed
300 ppm. The second phase of mineralisation occurs in
thin quartz veinlets, which in this case contain accessory
sphalerite, galena and pyrite. Where the veining is intense,
lead concentrations reach 7000 ppm and those of
zinc 1500 ppm, but these values persist over only a few
tens of cm of core. Finally, a low-temperature mineral
assemblage in which plumbogummite is dominant is
associated with the altered margins of dykes and gossanlike
zones occupying a north-south fault system. Lead
levels in the dyke margins range up to 1.5 % in zones
generally less than 50 cm thick, but 4.5 %I Pb has been
recorded in one specimen from the exposed gossan.
Fine stratiform pyrite iaminae in mudstone interbedded
with chert containing disseminated pyrite and
sphalerite suggests that at leas: some of the early
mineralisation is synsedimentary. Later mineralisation
phases are, however, structurally controlled and the
origin of the majority of the base metal mineralisation remains
problematical. The unusual abundance of minor
intrusions in the mineralised zone is strong circumstantial
evidence for an igneous source.
Full details of the soil geochemical surveys and the
geophysical surveys are available for inspection at the
Keyworth office of BGS
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