Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

Journal of the Geological Society

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Web of Science (3) Citing Articles via Google Scholar Google Scholar Articles by Liss, D. Articles by Hutton, D.H.W. Search for Related Content GeoRef GeoRef Citation

New palaeomagnetic results from the Whin Sill complex: evidence for a multiple intrusion event and revised virtual geomagnetic poles for the late Carboniferous for the British Isles

Department of Earth Sciences, University of Birmingham, Birmingham B15 2TT, UK (e-mail: dirk_liss@yahoo.co.uk)

A large-scale palaeomagnetic study (125 specimens from 88 sampling localities) has been carried out on the Whin Sill complex and its associated dykes in northern England. The dominant carrier of remanent magnetization of the doleritic rocks is relatively pure magnetite of pseudo-single domain size, and the characteristic remanent magnetizations are typically well defined and unidirectional. Regionally consistent palaeomagnetic directions are obtained from three geographically distinct parts of the Whin Sill complex, here named as the Holy Island Sill (Declination/Inclination (D/I)=189.5/–2.8, ₉₅=6.3), the Alnwick Sill (D/I=194.6/–25.6, ₉₅=8.1) and the Hadrian's Wall–Pennines Sill (D/I=189.2/3.3, ₉₅=3.5). Although the Holy Island Sill and the Hadrian's Wall–Pennines Sill are of similar age (c. 296 Ma) and indistinguishable on palaeomagnetic grounds, the difference in palaeomagnetic directions between them and the Alnwick Sill demonstrates the multi-component nature of the complex; magma-flow indicators suggest that the Holy Island Sill and the Hadrian's Wall–Pennines Sill may also represent separate intrusion events. Dykes local to the three sills have remanence directions corresponding to their respective sills and can tentatively be identified as their feeder dykes. Virtual geomagnetic poles for the three palaeomagnetic sites are: Holy Island Sill and Holy Island Dyke, 346.8E, 35.4S; Alnwick Sill, High Green Dyke and St. Oswald's Chapel Dyke, 337.1E, 47.1S; Hadrian's Wall–Pennines Sill and Hett Dyke, 347.1E, 32.9S.

KEYWORDS: sills, dykes, palaeomagnetism, emplacement, dolerite

This article has been cited by other articles:

				N.R. Goulty Emplacement mechanism of the Great Whin and Midland Valley dolerite sills Journal of the Geological Society, December 1, 2005; 162(6): 1047 - 1056. [Abstract] [Full Text] [PDF]