Resolution of regional fluid flow related to successive orogenic events on the Laurentian margin

Mark, D.F. , Parnell, J., Kelly, S.P. and Sherlock, S.C. (2007) Resolution of regional fluid flow related to successive orogenic events on the Laurentian margin. Geology, 35(6), pp. 547-550. (doi: 10.1130/​G23388A.1)

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Abstract

Seven localities distributed along a 180-km-long outcrop within the UK sector of the Laurentian margin were sampled, and all showed two phases of authigenic K-feldspar. The first phase was precipitated from a cool fluid of moderate salinity, and the second phase was precipitated from a hotter, more saline fluid. Ar-Ar ages for the two episodes of authigenesis are ca. 470 Ma and ca. 432 Ma. The data can be interpreted to represent two phases of regional-scale fluid migration related to Ordovician arc accretion and Silurian continent-continent convergence, corresponding to the Grampian and Scandian episodes of the Caledonian orogeny, respectively.

Item Type:Articles
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Mark, Professor Darren
Authors: Mark, D.F., Parnell, J., Kelly, S.P., and Sherlock, S.C.
College/School:College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Geology
Publisher:Geological Society of America
ISSN:0091-7613

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