Jones, R.C.; Beer, K.E.. 1990 Mineral investigations at Tredaule, near Launceston, Cornwall. Nottingham, UK, British Geological Survey, 53pp. (WF/90/005, Mineral Reconnaissance Programme report 113) (Unpublished)
Abstract
This report describes geochemical investigations commenced in the
vicinity of Tredaule, about lkm to the east of Altarnun and north of
the A30 road, but not comprehensively completed owing to logistical
problems.
Five sediment samples from the two small streams east of Tredaule
yielded panned concentrates with anomalous contents of both tin and
tungsten, suggestive of local mineralisation. A single soil sampling
traverse was sited parallel to the main stream and in the analyses of
34 soils from this line a small group of coincident tin and tungsten
anomalies were reported, as well as a marked pair of silver anomalies
farther to the south.
In an endeavour to determine the source of these anomalies a
gridded pattern of soil samples was collected over ground near Newhay
farm. A total of 379 samples were analysed for a range of ore metals
and associated elements. For some elements the results were combined
with those from the adjacent traverse line prior to statistical treatment.
From these combined results it is possible to recognise several
soils anomalous in tin, usually with associated elevated levels of
tungsten, and a different set anomalous in silver. The latter are
sometimes associated with anomalous levels of copper, but there is a
separate grouping of copper anomalies which may have closer relationships
either to the tin anomalies or to the volcanic rocks over which
they are located.
There remains an open question of whether the anomalies have been
fully defined in this restricted geochemical programme or whether they
continue to the east of the Tredaule stream through the fields where
sampling was not carried out. Because of this uncertainty it is
unwise to speculate too deeply upon the form of mineralisation giving
rise to the observed anomaly pattern, although the correlation between
tungsten and tin, and the location of their anomalies relative to
those of copper and to the mapped geology, is suggestive of an eastwest
hypothermal vein. A source for the silver anomalies is not
obvious.
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