Cilva Joseph

Cilva Joseph
  • Master of Science
  • PhD Candidate at Curtin University

About

5
Publications
604
Reads
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28
Citations
Introduction
My research is focused on the nanoscale study of xenotime and its potential geological applications using Atom Probe tomography and correlative microscopy.
Current institution
Curtin University
Current position
  • PhD Candidate
Additional affiliations
September 2018 - August 2019
Indian Institute of Technology Dhanbad
Position
  • Research Associate
Description
  • Petrogenesis of the ultramafic-mafic rock suites of the Sargur supracrustal belt in the Western Dharwar craton, Southern India: significance to the Archean crustal evolution. Hydrothermal vein-type magnesite deposit study.
Education
September 2016 - May 2018
Government College Kottayam
Field of study
  • Geology
August 2013 - June 2016
Government College Kottayam
Field of study
  • Geology

Publications

Publications (5)
Article
Constraining the age of many types of ore deposits remains challenging due to the lack of radiogenic isotopes incorporated into common ore-forming minerals. The timing of pre-Caledonian-hosted Cu mineralization along the entire ∼1200 km-long East Greenland Caledonides remains virtually unknown, hampering our knowledge of ore deposit timing and gene...
Conference Paper
Constraining precise ages for impact events is crucial in establishing Earth’s history, and several geochronometers have been developed to date impacts. We present electron backscatter diffraction (EBSD), sensitive high-resolution ion microprobe (SHRIMP) and atom probe tomography (APT) data from shocked xenotime [(Y,HREE)PO4] collected from two imp...
Article
This study focuses on the low-temperature mineralogical response of xenotime, a phosphate mineral routinely used as a geochronometer, to fluid-assisted alteration. The studied xenotime grain (z6413) comes from a ~1000 Ma pegmatite from the Grenville Province, Canada, and is commonly used as reference material for U-Pb analyses. At the microscale, t...
Article
Xenotime (YPO4) is an accessory phase common in low to high‐temperature geological environments. Xenotime is an established geochronometer, though its small size, low modal abundance, and textural complexity make it more difficult to analyse with traditional techniques but makes a prime candidate for nano‐scale analysis. In this study, we develop a...

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