Leake, Bernard Elgey, Singh, Dharm (1986) The Delaney Dome Formation, Connemara, W. Ireland, and the geochemical distinction of ortho- and para-quartzofeldspathic rocks. Mineralogical Magazine, 50 (356) 205-215 doi:10.1180/minmag.1986.050.356.03
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | The Delaney Dome Formation, Connemara, W. Ireland, and the geochemical distinction of ortho- and para-quartzofeldspathic rocks | ||
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
| Authors | Leake, Bernard Elgey | Author | |
| Singh, Dharm | Author | ||
| Year | 1986 (June) | Volume | 50 |
| Issue | 356 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_50/50-356-205.pdf+ | ||
| DOI | doi:10.1180/minmag.1986.050.356.03Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 3840 | Long-form Identifier | mindat:1:5:3840:3 |
| GUID | 0 | ||
| Full Reference | Leake, Bernard Elgey, Singh, Dharm (1986) The Delaney Dome Formation, Connemara, W. Ireland, and the geochemical distinction of ortho- and para-quartzofeldspathic rocks. Mineralogical Magazine, 50 (356) 205-215 doi:10.1180/minmag.1986.050.356.03 | ||
| Plain Text | Leake, Bernard Elgey, Singh, Dharm (1986) The Delaney Dome Formation, Connemara, W. Ireland, and the geochemical distinction of ortho- and para-quartzofeldspathic rocks. Mineralogical Magazine, 50 (356) 205-215 doi:10.1180/minmag.1986.050.356.03 | ||
| In | (1986, June) Mineralogical Magazine Vol. 50 (356) Mineralogical Society | ||
| Abstract/Notes | AbstractA number of geochemical plots are suggested by means of which metamorphosed quartzofeldspathic sedimentary rocks (meta-sandstones, meta-arkoses, quartzites, etc.) can be distinguished from their metamorphosed igneous mineralogical analogues (metarhyolite, meta-granite, etc.). These plots are applied to an enigmatic, partly mylonitized, quartzofeldspathic series, the Delaney Dome Formation, which is involved in a major thrust zone. The formation is shown to be igneous and is probably a meta-rhyolite. The plots proposed should have general application in identifying the precursors of both high-grade and low-grade quartzofeldspathic rocks of unknown origin. | ||
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