“…3). Recent palaeomagnetic data from France and Iberia (see Burrett, 1983a) places these areas in high palaeolatitudes of about 65 o S or more which is in accord with palaeoclimatic evidence (Spjeldnaes, 1967;Dor6 & Le Gall, 1972). The palaeomagnetic data from the Early Ordovician of the Shan-Thai block (Haille, 1980), which yield a palaeolatitude of 43°N must be viewed with scepticisim, as those data were derived from highly cleaved and thermally metamorphosed carbonates.…”