Sixteen small intrusions and one mineral occurrence were examined briefly for indications of disseminated mineralisation. Stream sediment and panned concentrate samples were collected from streams crossing some of the intrusions to supplement existing coverage, and geophysical surveys were conducted over Priestlaw, Cockburn Law and Lamberton Moor. Rock samples collected at some of the localities were analysed for major and trace elements. The intrusive rocks range in composition from granite to diorite and in grain size from hypabyssal to plutonic types. The larger intrusions at Portencorkrie, Priestlaw and Cockburn Law are zoned. Hydrothermal alteration, in places with associated pyrite, was recorded at Mains of Dhuloch, Mo...
Five boreholes in the vicinity of the ancient Ag-Ni-Pb mine at Hilderston, near Bathgate have yield...
A regional geochemical drainage reconnaissance programme was undertaken over 900 km2 of south-west S...
Fourteen inclined percussive drillholes have shown that weak tin mineralisation persists into the h...
Reconnaissance geochemical and geophysical surveys were carried out in the area of Culvennan Fell ...
A reconnaissance geochemical drainage survey of 720 km2 of Dalradian outcrop in central Argyll ide...
The subsurface characteristics of three known occurrences of fracture-controlled mineralisation in...
Reconnaissance soil sampling within the catchment of streams containing anomalous levels of copper...
Soil and stream sediment samples collected from fault zone and the already well-known (and to an ar...
The Fore Burn igneous complex consists mainly of quartz-microdiorite, tonalite and feldspar porphyr...
A co-ordinated geochemical-geophysical-geological investigation of copper mineralisation in the Mea...
Lower Carboniferous volcanics have been mapped and sampled in detail in an attempt to establish the...
A brief investigation of low-grade copper mineralisation associated with a small, talc-alkaline por...
Several narrow, lenticular belts of black cherty mudstone and siltstone (the Moffat Shales), altern...
Historical accounts of copper mining near Middleton Tyas in the 18th century show that small tonna...
Five areas on the outcrop of the Helsby Sandstone Formation (formerly Keuper Sandstone) and Tarpor...
Five boreholes in the vicinity of the ancient Ag-Ni-Pb mine at Hilderston, near Bathgate have yield...
A regional geochemical drainage reconnaissance programme was undertaken over 900 km2 of south-west S...
Fourteen inclined percussive drillholes have shown that weak tin mineralisation persists into the h...
Reconnaissance geochemical and geophysical surveys were carried out in the area of Culvennan Fell ...
A reconnaissance geochemical drainage survey of 720 km2 of Dalradian outcrop in central Argyll ide...
The subsurface characteristics of three known occurrences of fracture-controlled mineralisation in...
Reconnaissance soil sampling within the catchment of streams containing anomalous levels of copper...
Soil and stream sediment samples collected from fault zone and the already well-known (and to an ar...
The Fore Burn igneous complex consists mainly of quartz-microdiorite, tonalite and feldspar porphyr...
A co-ordinated geochemical-geophysical-geological investigation of copper mineralisation in the Mea...
Lower Carboniferous volcanics have been mapped and sampled in detail in an attempt to establish the...
A brief investigation of low-grade copper mineralisation associated with a small, talc-alkaline por...
Several narrow, lenticular belts of black cherty mudstone and siltstone (the Moffat Shales), altern...
Historical accounts of copper mining near Middleton Tyas in the 18th century show that small tonna...
Five areas on the outcrop of the Helsby Sandstone Formation (formerly Keuper Sandstone) and Tarpor...
Five boreholes in the vicinity of the ancient Ag-Ni-Pb mine at Hilderston, near Bathgate have yield...
A regional geochemical drainage reconnaissance programme was undertaken over 900 km2 of south-west S...
Fourteen inclined percussive drillholes have shown that weak tin mineralisation persists into the h...