Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-26T02:40:22.874Z Has data issue: false hasContentIssue false
  • English
  • Français

Discussion of ‘Silicified serpentinite – a residuum of a Tertiary palaeo-weathering surface in the United Arab Emirates’

Published online by Cambridge University Press:  18 June 2014

A. M. Lacinska  and
M. T. Styles
A. M. Lacinska
Affiliation:
British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottinghamshire NG12 5GG, UK; email: [email protected]
M. T. Styles
Affiliation:
British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottinghamshire NG12 5GG, UK
Get access Rights & Permissions [Opens in a new window]

Extract

Alicja M. Lacinska and Michael T. Styles reply: We appreciate the comment by C. R. M. Butt on the publication by Lacinska & Styles (2013) on the silicified serpentinites described from the Hajar Mountains in the United Arab Emirates. This comment is based on his very extensive knowledge of laterites and regoliths from ancient shield areas around the world; the degree to which this knowledge is directly applicable to the rocks formed at the margins of a recently uplifted mountain range, as described in the original paper, is debatable.

Type
Discussion
Information
Geological Magazine , Volume 151 , Issue 6 , November 2014 , pp. 1147
Copyright
BGS © NERC 2014 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Lacinska, A. M., Styles, M. T. & Farrant, A. R. 2014. Near-surface diagenesis of ophiolite-derived conglomerates of the Barzaman Formation, United Arab Emirates; a natural analogue for permanent CO2 sequestration via mineral carbonation of ultramafic rocks. In Tectonic Evolution of the Oman Mountains (eds Rollinson, H. R., Searle, M. P., Abbasi, I. A., Al-Lazki, A. & Kindi, M. H. Al), pp. 343–60. Geological Society of London, Special Publications no. 392.Google Scholar