Intrusion history of the Portrush Sill, County Antrim, Northern Ireland: Evidence for rapid emplacement and high-temperature contact metamorphism

Morgane Ledevin, Nicholas Arndt, Mark R. Cooper, Garth Earls, Paul Lyle, Charles Aubourg, Eric Lewin

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

The gabbroic Portrush Sill in Northern Ireland, part of the North Atlantic Igneous Province, intruded Lower Jurassic mudstones and siltstones about 55 Ma ago. We used petrologic observations and geochemical analyses to study how the sill interacted with the sedimentary rocks. Field relationships show that an Upper Sill and numerous associated Minor Intrusions were emplaced in the sedimentary host rocks before intrusion of the Main Sill, some 10 m above its upper contact. Geochemical analyses reveal two magma contamination processes: Nb and Ta anomalies, coupled with incompatible element enrichment, record contamination by deep crustal rocks, whereas Li, Pb and Ba anomalies reveal a superficial contamination through fluid circulation at the contact between magmatic and sedimentary rocks. Analysis of mineral assemblages and geochemical data from the contact aureole demonstrate uniform metamorphic conditions between the two main intrusions and an absence of a thermal gradient. The identification of pyrrhotite by magnetization analyses and of orthopyroxene by microprobe analyses indicates very high temperatures, up to 660 °C. Thermal modelling explains these temperatures as the coupled effects of the Main Sill and the earlier intruded Upper Sill and Minor Intrusions. Even though the chemical composition of the Main Sill suggests another type of parental liquid, all three units were emplaced in a very short time, certainly less than five years.

Original languageEnglish
Pages (from-to)67-79
Number of pages13
JournalGeological Magazine
Volume149
Issue number1
DOIs
Publication statusPublished - Jan 2012
Externally publishedYes

Fingerprint

contact metamorphism
sill
emplacement
history
sedimentary rock
anomaly
igneous province
aureole
crustal contamination
pyrrhotite
siltstone
orthopyroxene
magnetization
host rock
mudstone
Jurassic
chemical composition
liquid
fluid
mineral

Keywords

  • contact metamorphism
  • magma contamination
  • Northern Ireland
  • Portrush Sill
  • thermal modelling

ASJC Scopus subject areas

  • Geology

Cite this

Intrusion history of the Portrush Sill, County Antrim, Northern Ireland : Evidence for rapid emplacement and high-temperature contact metamorphism. / Ledevin, Morgane; Arndt, Nicholas; Cooper, Mark R.; Earls, Garth; Lyle, Paul; Aubourg, Charles; Lewin, Eric.

In: Geological Magazine, Vol. 149, No. 1, 01.2012, p. 67-79.

Research output: Contribution to journalArticle

Ledevin, Morgane ; Arndt, Nicholas ; Cooper, Mark R. ; Earls, Garth ; Lyle, Paul ; Aubourg, Charles ; Lewin, Eric. / Intrusion history of the Portrush Sill, County Antrim, Northern Ireland : Evidence for rapid emplacement and high-temperature contact metamorphism. In: Geological Magazine. 2012 ; Vol. 149, No. 1. pp. 67-79.
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