Palaeomagnetism is the study of the strength and direction of the Earth's magnetic field as it has changed over geologic time.
D. H. Tarling has written: 'Continental drift and biological evolution' -- subject(s): Continental drift, Evolution 'Palaeomagnetism' -- subject(s): Paleomagnetism 'Continental drift' -- subject(s): Continental drift 'Palaeomagnetism & Diagenesis in Sediments'
Serena Ann Jones has written: 'Palaeomagnetism as a tool for basin analysis'
Robert Foster Black has written: 'Palaeomagnetism of part of the Purcell system in southwestern Alberta and southeastern British Columbia' -- subject(s): Geology, Stratigraphic, Paleomagnetism, Stratigraphic Geology
Alfred Wegener was the proponent of the Continental Drift Theory. The scientific community accepted this theory due to the phenomena of paleomagnetism, sea floor spreading and plate tectonics.
Continental Drift was devised by Alfred Wegener. Evidence would be: 1. Deposition of glacial tills in the southern continents and how they match when connected together. 2. Location of terrestrial fossils e.g. Mesosaurus which fossils can be found in South America and Southern Africa which were once connected. 3. Locations of old mountain chains e.g. Caledonians. 4. Location of fossil deserts, swamps and salt lakes. 5. Palaeomagnetism where lava which contains iron which is magnetic solidified marking the position of magnetic north in the lava. When the rocks which were formed from the solidified magma it was found that the rocks didn't point to what is now magnetic north proving that the continents must have moved so that the rocks could have at one point pointed north.