Concomitant thrusting and magmatism resulted in the development of ductile mylonites in the Calamita Schists, part of the contact aureole of the Late Miocene Porto Azzurro pluton. This mylonite is made up of stretched and recrystallized quartz layers, interlayered with thin sericite-rich levels. Sericite resulted from the crushing of contact-metamorphic minerals such as andalusite, cordierite, …[Read More]
Hi Nadine, thanks for speaking with us today, can you tell us a little bit about your background and how you got to where you are now? Thank you for inviting me! I’m a geologist and the Assistant Curator of Fossil Mammals at the Natural History Museum, London. I studied MSci Geology at University College …[Read More]
Petrologists spend a large part of their time peering down microscopes at wafer thin slices of rock to work out what they’re made of and how they were formed. What lies on the other side of the lens can be an incredibly beautiful pattern, a kaleidoscope of colour, or stark bands of black and white, …[Read More]
