Imperial College London

ProfessorJamieWilkinson

Faculty of EngineeringDepartment of Earth Science & Engineering

Professor of Geology
 
 
 
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Contact

 

j.wilkinson Website

 
 
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Location

 

PA418Natural History MuseumNatural History Museum

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Summary

 

Publications

Citation

BibTex format

@inproceedings{Brugge:2017,
author = {Brugge, E and Wilkinson, J and Miles, A},
publisher = {SGA},
title = {Habit and Chemistry of Apatite at Chuquicamata, Chile},
year = {2017}
}

RIS format (EndNote, RefMan)

TY  - CPAPER
AB - Apatite is well suited to the study of porphyry systems. It occurs in both the magmatic and hydrothermal domains and the large range in possible trace element substitutions can reveal crystallisation conditions that reflect key events during porphyry formation. This project aims to use the trace element chemistry of apatite as a probe of porphyry development. A global study of apatite composition will aim to identify fingerprints which may be indicative of a fertile porphyry environment. Initial results from the Chuquicamata Cu-Mo porphyry, Chile reveal limited compositional differences in major and trace element compositions (Ca, P, Cl, Na, Mn, S, Se, Fe, Mg, Al, Si, La, Ce, Nd) between apatites of different habits that are interpreted to be magmatic in origin. However, vein-hosted and hydrothermally-altered apatite are compositionally distinct, probably controlled by strong fractionation of elements during separation of magmatic-hydrothermal fluids. This suggests potential for the future study of potassic alteration in porphyry systems using apatite.
AU - Brugge,E
AU - Wilkinson,J
AU - Miles,A
PB - SGA
PY - 2017///
TI - Habit and Chemistry of Apatite at Chuquicamata, Chile
ER -