How does recorded temperature changes upon impact shock? Anna Barbaro and co-authors estimated temperature by a graphite-thermometer based on micro-raman spectroscopy data, on 5 ureilitic fragments (FRO 95028, FRO 01089, FRO 97013, FRO 01088 and...
Read moreCharacterization of carbon phases in Yamato 74123 ureilite to constrain the meteorite shock history
Characterization of carbon phases in Yamato 74123 ureilite to constrain the meteorite shock history The formation and shock history of primitive achondrites meteorites such as ureilite has been debated for decades! The characterization of carbon...
Read moreImpact diamonds in ureilites by catalytic growth involving Fe-Ni-silicide
Impact diamonds in ureilites by catalytic growth involving Fe-Ni-silicide: The example of Kenna meteorite The occurrence of shock-induced diamonds in ureilite meteorites is common and is used to constrain the history of the ureilite parent...
Read moreCooling history and emplacement of a pyroxenitic lava as proxy for understanding Martian lava flows
Cooling history and emplacement of a pyroxenitic lava as proxy for understanding Martian lava flows Our PhD student Mara Murri at her second Scientific Reports paper for this year! Congratulations!! She has now concluded her studies on the...
Read moreQuantifying hexagonal stacking in diamond
Once again on the shock impact topic. In her new nice manuscript in Scientific Reports Mara Murri presents some of the recent considerations about structural disorder in the form of complex combinations of cubic and hexagonal stacking motifs...
Read moreViscosity experiments at superliquidus temperatures
Rheology is the key factor to understand dynamic processes and behavior of magma rising through volcanic conduit and lava emplacement on Earth or other terrestrial planets. Today we can monitor the evolution of magma and volcanic mixtures by...
Read moreExperimental validation of intracrystalline “geothermometry” for rocks
In this paper, we test the available experimental calibrations for clino and orthopyroxenes as geothermometer by determining their site in synthetic samples grown from a hydrous nepheline basanite in a piston-cylinder apparatus at 1050 °C at...
Read moreFinite Element modelling of stresses in inclusions by Mattia L. Mazzucchelli on Geology.
Check our our latest paper on Finite Element modelling of stresses in inclusions by Mattia L. Mazzucchelli on Geology. Elastic geothermobarometry on inclusions is a method to determine pressure-temperature conditions of mineral growth independent...
Read moreThermo-elastic behavior of grossular garnet
In her manuscript Sula Milani provides for the first time consistent the thermo-elastic parameters for grossular garnet using simultaneous fitting of pressure-volume-temperature data combined with either adiabatic (KS) or isothermal bulk modulus...
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