S-C mylonites developed in andalusite-cordierite micaschist (Calamita Schists) in the contact aureole of the Porto Azzurro pluton. The white layers are made of quartz, while the brown layers consist predominantly of white mica and biotite. Top-to-left (East) sense of shear. Read more: Papeschi et al (2017). Heterogeneous brittle-ductile deformation at shallow crustal levels under high thermal cond ...[Read More]
A Pedagogical Dance: EGU’s Teacher-Scientist Pairing Scheme
An email from Giuliana Panieri, a geology professor at the Arctic University of Norway (UiT) in Tromsø, cracked my pandemic bubble late last year. She invited me to join an unconventional expedition (AKMA OceanSenses) to the Arctic Ocean, where scientists worked hand-in-hand with other societal actors, to integrate different kinds of knowledge and create tools that help open up people’s minds to a ...[Read More]
Sustainable Energy Geoscientist reflects on UN’s COP27
This year, from 6 to 20 November, the United Nation’s COP27 took place in Sharm el-Sheikh in Egypt. The conference hosted several high-level and side events, key negotiations and press conferences, attended by more than 100 Heads of State and Governments and over 35,000 participants who deliberated climate action strategies around the world. I had the chance to speak with Dr Munira Raji about her ...[Read More]
Imaggeo On Monday: Computing for a blank globe
A tribute to the computational geosciences. A mix of computer infrastructure, a modern workstation, and a simple globe with coastlines. Found this scene at the back of room at Miraikan – the National Museum of Emerging Science and Innovation in Tokyo, Japan. The computers, screens, and globe are behind a plexi-glass and while not intended as part of an exhibition it almost becomes an art-mee ...[Read More]