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Record of fluid flow history through fractured conglomerates, Lower Old Red Sandstone of central Scotland

Martin Baron and John Parnell
Scottish Journal of Geology, 40, 145-157, 1 November 2004, https://doi.org/10.1144/sjg40020145
Martin Baron
Department of Geology and Petroleum Geology, Meston Building, University of Aberdeen, King’s College, Aberdeen, AB24 3UE (e-mail:)
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John Parnell
Department of Geology and Petroleum Geology, Meston Building, University of Aberdeen, King’s College, Aberdeen, AB24 3UE (e-mail:)
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Synopsis

Extensively fractured quartzite clasts in Lower Old Red Sandstone conglomerates adjacent to the Highland Boundary Fault Zone in central Scotland contain multiple populations of healed microfractures delimited by fluid inclusion planes. Microthermometric analysis indicates that the healing of microfractures oriented perpendicular to the trend of the Highland Boundary Fault Zone, which probably formed during Acadian overthrusting towards the SE along the fault zone in Middle Devonian times, involved moderate temperature (Th 102 to 238°C), low to moderate salinity (3 to 17 wt% NaCl eq.) aqueous fluids. The clasts also contain a second set of fluid inclusion planes oriented parallel to the Highland Boundary Fault Zone, which formed during extension associated with the intrusion of late Carboniferous quartz dolerite dykes. The healing of this set of microfractures involved low temperature (Th 58 to 155°C), low to moderate salinity (1 to 12 wt% NaCl eq.) aqueous fluids.

  • © 2004 Scottish Journal of Geology
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In this issue

Scottish Journal of Geology: 40 (2)
Scottish Journal of Geology
Volume 40, Issue 2
November 2004
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Record of fluid flow history through fractured conglomerates, Lower Old Red Sandstone of central Scotland

Martin Baron and John Parnell
Scottish Journal of Geology, 40, 145-157, 1 November 2004, https://doi.org/10.1144/sjg40020145
Martin Baron
Department of Geology and Petroleum Geology, Meston Building, University of Aberdeen, King’s College, Aberdeen, AB24 3UE (e-mail:)
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • For correspondence: [email protected]
John Parnell
Department of Geology and Petroleum Geology, Meston Building, University of Aberdeen, King’s College, Aberdeen, AB24 3UE (e-mail:)
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • For correspondence: [email protected]

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Record of fluid flow history through fractured conglomerates, Lower Old Red Sandstone of central Scotland

Martin Baron and John Parnell
Scottish Journal of Geology, 40, 145-157, 1 November 2004, https://doi.org/10.1144/sjg40020145
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  • Article
    • Synopsis
    • Introduction
    • Regional geology
    • Fractured Lower ORS conglomerates
    • Methodology
    • Orientations and morphologies of FIPs within fractured Lower ORS conglomerate quartzite clasts
    • Fluid inclusion data
    • Discussion
    • Conclusions
    • Acknowledgements
    • References
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