| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Paragenesis of hydrothermal mineralization in amphibolites and granulites around Porthkerris Point, the Lizard, Cornwall |
|---|
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
|---|
| Authors | Seager, A. F. | Author |
|---|
| Year | 1978 (December) | Volume | 42 |
|---|
| Page(s) | 509-511 | Issue | 324 |
|---|
| Publisher | Mineralogical Society |
|---|
| Download URL | https://rruff.info/doclib/MinMag/Volume_42/42-324-509.pdf+ |
|---|
| DOI | doi:10.1180/minmag.1978.042.324.15Search in ResearchGate |
|---|
| Mindat Ref. ID | 2967 | Long-form Identifier | mindat:1:5:2967:8 |
|---|
|
| GUID | 2cee5da7-d468-4698-9425-dfb5e4514451 |
|---|
| Full Reference | Seager, A. F. (1978) Paragenesis of hydrothermal mineralization in amphibolites and granulites around Porthkerris Point, the Lizard, Cornwall. Mineralogical Magazine, 42 (324) 509-511 doi:10.1180/minmag.1978.042.324.15 |
|---|
| Plain Text | Seager, A. F. (1978) Paragenesis of hydrothermal mineralization in amphibolites and granulites around Porthkerris Point, the Lizard, Cornwall. Mineralogical Magazine, 42 (324) 509-511 doi:10.1180/minmag.1978.042.324.15 |
|---|
| In | (1978, December) Mineralogical Magazine Vol. 42 (324) Mineralogical Society |
|---|
| Abstract/Notes | A study of the post-metamorphic hydrothermal mineralization in the gabbros of the Lizard has already been published (Seager, 1971). The present paper extends the investigation of mineralization in the peninsula to an adjacent area, on the NE. coast around Porthkerris Point. Table 1 gives the more important events of the paragenesis. Calcite and adularia are the only common minerals; all others are scarce or rare.The calcite that precedes and succeeds adularia is called early calcite and late calcite, respectively. Both early and late calcite occur in several generations differing in habit, fluorescence, and phosphorescence. |
|---|
These are possibly similar items as determined by title/reference text matching only.
