MSG Research in Progress Videos 2023

The main activity by MSG was to host the annual ‘Research in Progress’ meeting, which was held at the University of Oxford on 4–5th April, with an ice-breaker event on the 3rd April. The meeting was held as a hybrid event, and well attended, with 69 people in person, and 20 people joining online. In total, 16 countries were represented.

Forty-one talks were given across the two days, covering a range of topics including kinetics, petrochronology, and traditional regional studies of metamorphic terranes. Keynote talks were given by Donna Whitney (University of Minnesota, USA) and Iwona Klonowska (AGH University of Science and Technology, Poland), with Frank Spear (Rensselaer Polytechnic Institute, USA) giving the Barrow award winner’s talk. All keynote and award winner presenters attended the event in person. Maria Margarita Ariza-Acero (University of Lausanne, Switzerland) was awarded the student talk prize. A poster session was also held on the final evening, comprising sixteen posters. Omar Droubi (Penn State, USA) was awarded the student poster prize. The international nature of all keynotes and student prizes speaks to the increasing international profile that MSG has received following successful online conferences during COVID.

Thanks to Zeiss for sponsoring the ice-breaker event and the student poster prize. Thanks also to Richard Palin (University of Oxford) for being the lead organiser. Freya George has offered to host MSG at Bristol University in 2024; this will be discussed at our next committee meeting on 10th May 2024.

We also held an AGM at the RiP meeting. The only change to the committee was that Nicholas Lucas (University of Cambridge) replaced Isabel Carter (AGH-UST, Poland) as student representative and webmaster. 

MSG 2023 RiP conference, St Anne’s College, Oxford

Below are links to recordings of some of the presentations made during the meeting.

Barrow Award

Spear. The rocky road to equilibrium

Petrochronology

Kersley et al. Monazite: fast or slow growth in metamorphic rocks?
Webb et al. Re-Os molybdenite dating from the Tomnadashan Mine: wider implications for metallogeny around Loch Tay, Scotland
Connop et al. Timescales of continental lower crust formation: constraints from garnet Lu-Hf geochronology (Ivrea-Verbano Zone, Italy)
Corvò et al. Crystal plasticity and small fluid amounts govern the ability of titanite to record the age of deformation: the case of the Anzola shear zone (NE Italy)
Whitney et al.  (ABRIDGED) Sediment v. serpentinite in subducted slabs: fluid sources tracked by lawsonite composition in blueschist and eclogite

Petrochronology (2), modelling techniques, and petrological resources

Searle et al. Subduction initiation metamorphism: evidence from the Metamorphic Sole of the Oman Ophiolite

High-grade metamorphism and melting

Dominguez et al. Modelling melt production and extraction in the deep crust: case study of the El Oro Complex in Ecuador

Regional studies

Cesare et al. Contact metamorphism of graphitic semipelites constrains the depth of emplacement of the Re di Castello intrusion (Adamello Batholith)
Lucas et al. Enigmatic Grenville-aged eclogites in the Glenelg Inlier, NW Scotland
Petroccia et al. Metamorphic constraints in low-grade metapelites: a case from the Variscan belt in Sardinia
Wicker et al. Tectonic and metamorphic evolution of the high-pressure Quartzite-Phyllite Unit in the Aegean forearc, Peloponnese, Greece
Wheeler et al. Genesis of porphyry copper deposits: key roles for plagioclase and anhydrite in metasomatism
Cawood et al. P-T-t-D history of the Suru Valley, NW India: insights into the early evolution of the Himalayan orogen

Metamorphic processes

Tamblyn et al. Hydration and metamorphism of komatiites as a source for water for TTG formation in the Archean
Adak and Dutta. Reaction textures in ultramafic rocks: Evidence for supra to sub solidus reaction continuum
Gosselin et al. (Un)reliability of the Zr-in-titanite thermometer at low temperature (<600 °C)
Pattison. Problems with Barrovian metamorphism
Smye. How are sediments incorporated into continental lower crust?