Cora A. McKenna

ORCID: 0000-0003-0946-0639
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • Geochemistry and Elemental Analysis
  • Heavy metals in environment
  • X-ray Diffraction in Crystallography
  • Geology and Paleoclimatology Research
  • Crystallization and Solubility Studies
  • Geological formations and processes
  • Radioactive element chemistry and processing
  • earthquake and tectonic studies
  • Water-Energy-Food Nexus Studies
  • Analytical chemistry methods development
  • Lanthanide and Transition Metal Complexes
  • Water management and technologies
  • Petroleum Processing and Analysis
  • Paleontology and Stratigraphy of Fossils
  • Mineralogy and Gemology Studies
  • Radioactive contamination and transfer
  • Geological Studies and Exploration
  • Peptidase Inhibition and Analysis
  • Fungal Plant Pathogen Control
  • Hydrocarbon exploration and reservoir analysis
  • Groundwater and Watershed Analysis
  • Geomagnetism and Paleomagnetism Studies
  • Water resources management and optimization

Trinity College Dublin
2015-2022

22q11 Ireland
2016

University College Dublin
2016

University College Cork
2010

National University of Ireland
2010

Large igneous provinces (LIPs) have recently been suggested to originate at the edges of low-velocity zones on core mantle boundary (Plume Generation Zones). If true, LIPs can potentially be used constrain paleolongitude in plate tectonic reconstructions. To validate hypothesis, it is essential study which constrained by other methods, such as hotspot reference frames. An ideal candidate this end early Cenozoic North Atlantic Igneous Province (NAIP). Despite being largest volcanic unit...

10.1111/j.1365-246x.2010.04620.x article EN Geophysical Journal International 2010-05-01

Abstract We investigate the trace element and U‐Pb systematics of apatite 19 samples metapelites calcareous from two progressive metamorphic sequences Central Alps to further understanding behavior stability during metamorphism. data were acquired mineral separates by LA‐Q‐ICP‐MS. The explored using chondrite‐ whole‐rock normalized multielement plots principal component analysis biplots. Apatite rare earth (REE) U contents increase with increasing grade due competing growth/dissolution...

10.1029/2019gc008359 article EN Geochemistry Geophysics Geosystems 2019-07-31

Olivine offers huge, largely untapped, potential for improving our understanding of magmatic and metasomatic processes. In particular, a wealth information is contained in rare earth element ( REE ) mass fractions, which are well studied other minerals. However, data olivine scarce, reflecting the difficulty associated with determining fractions low ng g −1 range controlling effects LREE contamination. We report an analytical procedure measuring s using laser ablation quadrupole‐ ICP ‐ MS...

10.1111/ggr.12157 article EN Geostandards and Geoanalytical Research 2016-11-18

Eu(<sc>iii</sc>) can incorporate into the structure of selected uranyl minerals, as shown emission and vibrational spectroscopy.<sup>241</sup>Am(<sc>iii</sc>) tracer studies have been conducted, which has implications for migration Am(<sc>iii</sc>) in an underground repository containing SNF.

10.1039/c6dt00199h article EN cc-by Dalton Transactions 2016-01-01

Abstract The minor and trace element composition of minerals provides critical insights into a variety geological processes. Multi-element mapping by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) is an important technique applied for this purpose although the method rapidly advancing, there remains fundamental compromise between spatial resolution, detection limit, experiment duration when using sequential mass analyzers. To address limitation limited analyte...

10.2138/am-2022-8168 article EN American Mineralogist 2022-02-02
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