| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Chemical and Mineralogical Changes Associated with the Laxfordian Metamorphism of Dolerite Dykes in the Scourie-Loch Laxford Area, Sutherland, Scotland |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Burns, D. J. | Author |
|---|
| Year | 1966 (February) | Volume | 103 |
|---|
| Issue | 1 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s001675680005038xSearch in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 249595 | Long-form Identifier | mindat:1:5:249595:2 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Burns, D. J. (1966) Chemical and Mineralogical Changes Associated with the Laxfordian Metamorphism of Dolerite Dykes in the Scourie-Loch Laxford Area, Sutherland, Scotland. Geological Magazine, 103 (1) 19-35 doi:10.1017/s001675680005038x |
|---|
| Plain Text | Burns, D. J. (1966) Chemical and Mineralogical Changes Associated with the Laxfordian Metamorphism of Dolerite Dykes in the Scourie-Loch Laxford Area, Sutherland, Scotland. Geological Magazine, 103 (1) 19-35 doi:10.1017/s001675680005038x |
|---|
| In | (1966, February) Geological Magazine Vol. 103 (1) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | AbstractChemical analyses of dolerites and metadolerites from the Scourie-Loch Laxford area have been made, together with analyses of amphiboles and a pyroxene from these rocks.Chemical variation within the dykes as originally emplaced has been investigated. Introduction of material during metamorphism is limited, only potassium showing a marked increase in concentration. In the least-altered dykes a relationship between degree of clouding in felspar and amount of H2O+ present is indicated.Chemical analyses and optical properties of amphiboles show no distinctive trends which could be associated with the progress of the metamorphism. |
|---|
These are possibly similar items as determined by title/reference text matching only.
