|
|
|
|||||||||||||||||
| Journal of the Geological Society | ![]() |
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Article |
Department of Geology, Leicester University, Leicester LE1 7RH, UK
Palaeocurrents from the northernmost Aberystwyth Grits Formation are consistently from the north, which is at variance with the generally accepted southerly source area for the rest of the formation. The anomalous directions appear to indicate a structural high and possible sediment source to the north.
This article has been cited by other articles:
![]() |
R. Smith Turbidite systems influenced by structurally induced topography in the multi-sourced Welsh Basin Geological Society, London, Special Publications, January 1, 2004; 222(1): 209 - 228. [Abstract] [PDF] |
||||
![]() |
T. McCann Petrological and geochemical determination of provenance in the southern Welsh Basin Geological Society, London, Special Publications, January 1, 1991; 57(1): 215 - 230. [Abstract] [PDF] |
||||
![]() |
Discussion on the palaeocurrent evidence of a northern structural high to the Welsh Basin during the Late Llandovery Journal of the Geological Society, October 1, 1990; 147(5): 885 - 891. [Abstract] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |