nerc.ac.uk

The Northern Belt 100 years on : a revised model of the Ordovician tracts near Leadhills, Scotland

Smith, R.A.; Phillips, E.R.; Floyd, J.D.; Barron, H.F.; Pickett, E.A.. 2000 The Northern Belt 100 years on : a revised model of the Ordovician tracts near Leadhills, Scotland. Transactions of the Royal Society of Edinburgh (Earth Sciences), 91 (3-4). 421-434. 10.1017/S0263593300008270

Before downloading, please read NORA policies.
[thumbnail of northern_belt_paper.pdf]
Preview
Text
northern_belt_paper.pdf

Download (122kB) | Preview

Abstract/Summary

A new model for the provenance, depositional environment and tectonic setting of the Northern Belt of the Southern Uplands is presented. This turbiditic sandstone dominated sequence was deposited in a sand-rich submarine fan environment, overlying hemipelagic mudstones. The oldest sandstones are rich in juvenile ophiolitic material and record the first clastic input into the Southern Uplands basin. The bulk of the Northern Belt sedimentary sequence, however, is dominated by relatively quartzose sandstones derived from a Proterozoic continental/metamorphic source represented by the Midland Valley terrane of Scotland and Ireland. The quartzose dominated sequence was punctuated by the input of fresh volcanic detritus shed from a oceanic/continental island-arc situated to the W/NW of the Southern Uplands basin, with sediment dispersal turning to the NE along the axis of the basin in Scotland. The tectonic setting of the Southern Upland basin remains uncertain. The complex provenance of the sandstones and recognition of major olistostrome units within the Northern Belt succession suggest that it was tectonically active. The onset of clastic deposition within the Southern Uplands broadly corresponds to ophiolite obduction in both Scotland and Ireland, possibly in response to collision of a Cambrian-early Ordovician island-arc system with the Laurentian continental margin. If this interpretation is correct then the possibility arises that the Southern Uplands-Midland Valley terranes record the dismembering of this island-arc complex within an overall transpressional regime.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1017/S0263593300008270
Programmes: BGS Programmes > Geology and Landscape Northern
NORA Subject Terms: Earth Sciences
Date made live: 09 Aug 2012 12:56 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/19113

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...