Moreton, S.; Green, D. I. and Tindle, A. G.
Due to copyright restrictions, this file is not available for public download
|Google Scholar:||Look up in Google Scholar|
Hollandite and cryptomelane occur as intergrown botryoidal masses with goethite in a quartz vein hosted by the Leinster Granite at Cloghleagh Mine, near Blessington, Co. Wicklow. Coronadite and romanÃ¨chite accompany pyromorphite in an oxidised Pb–Znï¿½quartz vein at Old Luganure Mine, Glendasan, also in the Leinster Granite. Quantitative analyses show the Cloghleagh material to consist of bands of varying K:Ba ratio ranging from cryptomelane (K > Ba) to hollandite (Ba > K), but neither approaches end member composition. The Luganure material is mostly coronadite of near Pb-end member composition, in some cases mixed, or intergrown with, romanÃ¨chite.
|Item Type:||Journal Article|
|Copyright Holders:||2006 Royal Irish Academy|
|Academic Unit/Department:||Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Elizabeth Lomas|
|Date Deposited:||23 Feb 2009 15:45|
|Last Modified:||06 Aug 2016 07:05|
|Share this page:|