Thermal metamorphism of the Silurian strata of the Oslo region, assessed by conodont colour
- 1 July 1984
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 121 (4), 347-349
- https://doi.org/10.1017/s0016756800029241
Abstract
The colours of conodont elements recovered from Silurian limestones in the Oslo region, Norway, range from brown to grey. Samples from the south of the region contain black and grey conodonts, indicative of high palaeotemperatures. There is a general decrease in thermal metamorphism towards the north, with the lowest palaeotemperatures recorded from Toten, Ringsaker and parts of the Ringerike district. There is a close correlation between thermal metamorphism and the proximity of Permian intrusions.Keywords
This publication has 2 references indexed in Scilit:
- Marine incursion in Upper Palaeozoic sedimentary rocks of the Oslo Region, Southern NorwayGeological Magazine, 1981
- Conodonts as paleotemperature tools in Ordovician rocks of the Caledonides and adjacent areas in Scandinavia and the British IslesGeologiska Föreningen i Stockholm Förhandlingar, 1980