3-D Modeling of the Lisheen and Silvermines Deposits, County Tipperary, Ireland: Insights into Structural Controls on the Formation of Irish Zn-Pb Deposits
|Title:||3-D Modeling of the Lisheen and Silvermines Deposits, County Tipperary, Ireland: Insights into Structural Controls on the Formation of Irish Zn-Pb Deposits||Authors:||Kyne, Roisin; Torremans, Koen; Güven, John; Doyle, Robert; Walsh, John J.||Permanent link:||http://hdl.handle.net/10197/10857||Date:||1-Feb-2019||Online since:||2019-07-08T09:47:20Z||Abstract:||Faults are important structures in the formation of many mineral deposits, often acting as conduits for ore-forming fluids and sometimes providing, or generating, the bounding structures to associated mineralizing sites. Using 3-D analysis and modeling of the Lisheen and Silvermines deposits within the Irish ore field, we investigate the geometry of normal fault systems and their implications on the origin and nature of associated deposits. These Irish-type deposits are carbonate hosted and developed within the hanging walls of normal faults arising from an Early Carboniferous episode of north-south rifting, with relatively limited amounts of later deformation. Structural analysis of high-quality mine datasets indicates that fault segmentation is ubiquitous with left-stepping segments arising from north-south stretching developed above generally ENE-NE-trending fault arrays, which are subparallel to older Caledonian penetrative fabrics and structure within underlying Silurian and Ordovician rocks. Fault segments occur on different scales and have a profound impact on structural evolution, with larger scale segments and intervening relay ramps defining distinct orebodies within deposits and smaller scale segments and relays potentially providing paths for upfault fluid flow. The difference in behavior is attributed to the integrity of associated relay ramps where intact ramps represent orebody-bounding structures, and smaller breached ramps provide enhanced associated hydraulic properties and act as vertical conduits. Hanging-wall deformation along the rheological boundary between host-rock limestones and underlying shales has an important control on the localization of earlier dolomitization and/or brecciation and later mineralization adjacent to this contact, and on the migration pathways for basinal brines and mineralizing fluids.||Funding Details:||European Commission Horizon 2020
European Commission - Seventh Framework Programme (FP7)
Science Foundation Ireland
|Type of material:||Journal Article||Publisher:||Society of Economic Geologists||Journal:||Economic Geology||Volume:||114||Issue:||1||Start page:||93||End page:||116||Copyright (published version):||2019 the Authors||Keywords:||Ireland; Brines; Lead ores; Mineral deposits; Paleozoic; Structural analysis; Lead-zinc deposits; Metal ores; Zine ores; Plate tectonics||DOI:||10.5382/econgeo.2019.4621||Language:||en||Status of Item:||Peer reviewed|
|Appears in Collections:||Earth Sciences Research Collection|
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