by John | Jan 31, 2024 | Bouguer
It took a few years for the significance of the linear magnetic anomalies discovered by Ron Mason and Arthur Raff to be realised, but they were key factors in the development of Plate Tectonics. This development might have been considerably delayed if their work, arguably the first systematic magnetic survey of a large area of oceanic crust, had instead been carried out over the seas east of Queensland. Even today the uniform data set that provides the best approach to study of this region is gravitational, not magnetic.
by John | Dec 31, 2023 | Bouguer
Back in the mid-1960s, plate tectonics was still in its infancy but the origin of the shallow rises in the Tasman Sea, as strips of Australia peeled away like layers on an onion, was already pretty obvious. Inevitably, there was speculation on possible links between ophiolites in eastern Papua and New Caledonia.
by John | Nov 30, 2023 | Bouguer
Giving a talk in the AGH university building in Krakow was memorable, as far as I was concerned, because it was the building where Eddie Polak, one of my first geophysical mentors, studied during the four years that preceded the invasion of Poland and the start of the Second World War. I was able to imagine him in his time there all the better because he had left me with a typescript of his memoirs.
by John | Oct 31, 2023 | Bouguer
On 9 October, GNS Science, which is effectively New Zealand’s geological survey organisation, made a startling announcement. “Zealandia”, so its publicity department contended “just became the first continent to be completely mapped”. But what is Zealandia, and are these extravagant claims justified?
by John | Sep 30, 2023 | Bouguer
The world of scientific publishing is coming in for a lot of criticism these days, and rightly so in many cases. But are scientists not in some respects their own worst enemies, making rods for their own backs by custom and convention rather direct outright instruction?
by John | Sep 4, 2023 | Bouguer
In the late 1990s the European Science Foundation, taking advantage of the new possibilities for scientific interchange and fieldwork in a Europe no longer divided by an Iron Curtain, sponsored an international programme known as PANCARDI within which geologists and geophysicists from the countries of the Carpathian and Dinaric orogens and the Pannonian Basin came together to exchange information and reach a better understanding of the evolution through time of that very complex region. Is it not time for a second such programme?
