Leake, R.C.; Cameron, D.G.; Bland, D.J.; Styles, M.T.. 1990 Gold and platinum group elements in drainage between the River Erme and Plymouth Sound, south Devon. Nottingham, UK, British Geological Survey, 66pp. (WF/90/003, Mineral Reconnaissance Programme report 111) (Unpublished)
Abstract
Significant amounts of gold have been found in drainage sediment at
several localities in the area between the estuary and lower part of the
River Erme and Plymouth Sound in south Devon. Gold is particularly
abundant at a site about 2 km to the southwest of Holbeton where many of
the grains are dendritic or otherwise extremely irregular in shape. The
dendritic gold shows internal zonation of Pd abundance very similar to
that seen in material within carbonate veins in limestone at Hope's
Nose, Torquay. Other grains show incomplete rims rich in Pd (up to 13%)
or are close to pure gold in composition. Grains with silver-rich rims
are much less common than in drainage and overburden samples from east
of the River Erme. Associated with the dendritic gold from southwest of
Holbeton are dendritic, elongate knobbly and subrounded grains rich in
either Pt or Pd or both, forming around 5% of the total. Though some
grains are either pure potarite (PdHg) or Au-bearing potarite without
significant internal compositional variation, the majority, including
all those containing a significant amount of Pt, show very complex
compositional zonation. Six PGE-bearing compositional types have
provisionally been recognised. The cores of grains are generally Au-rich
either Au with minor contents of other metals or Au with significant Pd
and Hg. Rims are generally Pt-rich, often with a significant Au or Cu
content which may be recognisable as a distinct thin zone. Other
compositions include Pt with a significant Hg content and a combination
of roughly equal amounts of Pd, Hg, Au and Pt. Some grains show clear
concentric zonation and there may be very major compositional
differences between zones only a few microns thick.
Cinnabar occurs in small amounts in several drainage samples from the
area but is particularly abundant (up to 2000 ppm Hg) in samples derived
from an area underlain by Middle Devonian chiefly mafic volcanic rocks
in the northeast of the area. The distribution of
Mg,Ca,Ti,Mn,Fe,S,Ni,Cu,Zn,As,Rb,Zr,Sn,Sb,Ba, W,Pb and Bi in drainage
samples is also discussed. Au concentrations show greatest positive
correlation with Mn and Fe but a correlation with Sn is also
significant.
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