Jet. Channell et al., PALEOMAGNETIC STUDY OF LIANDOVERY (LOWER SILURIAN) RED BEDS IN NORTH-WEST ENGLAND, Geophysical journal international, 115(3), 1993, pp. 1085-1094
High unblocking temperature magnetization components carried by haemat
ite have been isolated from 12 sites of Llandovery (Lower Silurian) re
d mudstones from NW England. The principal deformation phase in this a
rea is Acadian (mid-Devonian), however, some faults (with related fold
s) were also active during the later Variscan orogeny. The site-mean m
agnetization directions pass a regional fold test at the 95 per cent c
onfidence level, implying that the magnetization components pre-date A
cadian folding. The overall mean direction (Declination: 43.4-degrees,
Inclination: -24.1-degrees, alpha95: 12.4-degrees) gives a pole posit
ion at 13.6-degrees-S, 313.9-degrees-E and a palaeolatitude of 12-degr
ees-S. The low palaeolatitude implies closure of the Iapetus Ocean bet
ween Eastern Avalonia and Laurentia by Late Llandovery time and is con
sistent with a recently published palaeolatitude (13-degrees-S) for th
e Wenlock (mid-Silurian) of southern Britain. Comparison of these valu
es with the published palaeolatitude from NW England of 43-degrees-S f
or Caradoc (Late Ordovician) time implies very rapid (at least 15 cm y
r-1) northward drift of Eastern Avalonia during Late Ordovician/Early
Silurian time. The new pole position from the Llandovery red beds lies
close to Late Silurian and Early Devonian poles from Scotland and Wal
es, but is significantly different from a group of mid-Silurian poles
comprising data from Scottish intrusions and from Swedish sediments. T
his discrepancy may be due to Late Silurian/Early Devonian (pre-Acadia
n) remagnetization of our sampling sites, or local clockwise rotation
of the sampling sites during Acadian and/or Variscan deformation. Howe
ver, the positive fold test, presence of reversals and local deformati
on history tend to mitigate against these possibilities. The more like
ly interpretation is that although Baltica/Scotland were one continent
al block from the mid-Silurian (Scandian orogeny), Eastern Avalonia di
d not become part of this block until latest Silurian.