Macro to micro-scale insights into granite petrogenesis; a case study from the Caledonian Ross of Mull granite (ROMG), Argyllshire, Northwest Scotland
dc.check.embargoformat | Embargo not applicable (If you have not submitted an e-thesis or do not want to request an embargo) | en |
dc.check.info | Not applicable | en |
dc.check.opt-out | Not applicable | en |
dc.check.reason | Not applicable | en |
dc.check.type | No Embargo Required | |
dc.contributor.advisor | Reavy, John | en |
dc.contributor.advisor | Finch, Adrian | en |
dc.contributor.advisor | Gamble, John | en |
dc.contributor.author | Zaniewski, Adam | |
dc.contributor.funder | University College Cork | en |
dc.contributor.funder | European Commission | en |
dc.date.accessioned | 2018-09-04T11:53:51Z | |
dc.date.available | 2018-09-04T11:53:51Z | |
dc.date.issued | 2018 | |
dc.date.submitted | 2018 | |
dc.description.abstract | The Ross of Mull Granite (ROMG) occupies the largest part of the Pre-Paleogene inlier of the Ross of Mull peninsula, Isle of Mull, Argyllshire, Scotland and is the most south-westerly of the Northwest Highland Caledonian granitoid complexes. Re-mapping of the entire intrusion (Zaniewski et al. 2006) has revealed a reverse zonation of facies resulting from mafic-felsic magma interaction prior to ascent at the proposed intersection of the Sound of Iona Fault and Great Glen Fault with north-eastward emplacement of flattish sheets into high-grade lithologies of the Moine Supergroup. Subsequent to mapping, Quantitative X-Ray Diffractometry (QXRD) has re-enforced modal classifications of Zaniewski et al. (2006). To further examine if this phenomenon is also encoded at the micro-scale (crystal), and if a correlation exists with macro-scale (field) studies, in-situ elemental and Pb-Pb isotopic zoning in magmatic feldspars from all ROMG components were analysed. The following micro-scale studies have been undertaken: (a) detailed textural study of feldspars using cold Cathodo-Luminescence (CL) and Back-Scatter Electron (BSE) imaging; (b) acquisition of feldspar major and minor element abundances by Electron Probe Micro Analysis (EPMA) and Pb-Pb isotopes by Laser Ablation Multicollector Inductively Coupled Plasma Mass Spectrometry (LA-MC-ICP-MS). Feldspars throughout the components display a three-fold CL magmatic zonation associated with dissolution at the core followed by elemental spike zones of Ba, Sr (0.00 - 1.00 wt. %) and Ab [mol. %] with elemental re-equilibration back towards the rims. Such resorption surfaces correspond to rim-ward increase of 206Pb/204Pb and 208Pb/204Pb in alkali feldspars in host granitoid and andesine in early phase MME advocate dissolution attributed to punctuated mafic magmatic recharge from a mantle-derived component interacting with a crustal component. Bulk Pb-Pb isotope data also highlight the importance of magma mixing and mingling in the petrogenesis of the complex and define a simple binary mixing array reflecting quasi-contemporaneous hybridisation between such components. A temporal sequence of macro-scale and micro-scale events is proposed and it is evident that the process of mafic-felsic magma interaction seen at the outcrop-scale is encoded at the crystal-scale. | en |
dc.description.status | Not peer reviewed | en |
dc.description.version | Accepted Version | |
dc.format.mimetype | application/pdf | en |
dc.identifier.citation | Zaniewski, A. 2018. Macro to micro-scale insights into granite petrogenesis; a case study from the Caledonian Ross of Mull granite (ROMG), Argyllshire, Northwest Scotland. PhD Thesis, University College Cork. | en |
dc.identifier.endpage | 286 | en |
dc.identifier.uri | https://hdl.handle.net/10468/6704 | |
dc.language.iso | en | en |
dc.publisher | University College Cork | en |
dc.relation.project | European Commission (Marie Curie Fellowship) | en |
dc.rights | © 2018, Adam Zaniewski. | en |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/ | en |
dc.subject | Caledonian | en |
dc.subject | Granite petrogenesis | en |
dc.subject | Ross of Mull granite | en |
dc.thesis.opt-out | false | |
dc.title | Macro to micro-scale insights into granite petrogenesis; a case study from the Caledonian Ross of Mull granite (ROMG), Argyllshire, Northwest Scotland | en |
dc.type | Doctoral thesis | en |
dc.type.qualificationlevel | Doctoral | en |
dc.type.qualificationname | PhD | en |
ucc.workflow.supervisor | j.reavy@ucc.ie |
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