Diamonds are usually thought of as products of the deep Earth, crystallising under enormous static pressure far below our feet. But some diamonds form somewhere far stranger: in space! Until now, however, extraterrestrial diamonds were assumed to...
Read moreNew EoS for almandine and spessartine garnets!
To address the sparse and inconsistent thermal expansion data previously available for almandine and spessartine garnets, this study “Revised PVT equations of state for almandine and spessartine garnets: implications for...
Read moreExploring the stiffening of quartz and its effect on the strain-stress relationship
When minerals are entrapped within host minerals during high-pressure and high-temperature metamorphic processes, their residual stress state serves as an elastic geobarometer to reconstruct their initial entrapment conditions. Traditional models...
Read moreQuartz in Garnet Isn’t Always Stressed—It’s Just Under Tension!
Elastic thermobarometry using quartz inclusions in garnet (QuiG) faces reliability issues in high-temperature terranes due to tensile strain. To investigate this problem, the authors analysed QuiG results from Adirondack metapelites alongside...
Read moreNew features in Crystal Palace: uncertainties for recalculated bond lengths, angles and polyhedral volumes! Now it’s Crystal Clear!
Crystal Palace is a program designed to automate the organization and analysis of refined crystal structures from parametric studies (varying pressure, temperature, or composition) using CIF files, eliminating the risks of manual data entry for...
Read moreMeet RamanCrystalHunter: The New Standard for Raman Spectroscopy Analysis
Stop struggling with messy Raman baselines! 💎 Fabrizio Nestola and team have just released RamanCrystalHunter (RCH)—a free, all-in-one software designed to take the headache out of mineral identification. Whether you’re analyzing complex...
Read moreOmphacite’s Hidden Clues: A Step Forward in Raman Geobarometry
Omphacite’s Hidden Clues: A Step Forward in Raman Geobarometry Omphacite, a mineral commonly trapped inside garnet, could be a powerful tool for Raman elastic geobarometry—a technique that helps scientists determine the pressures ancient...
Read moreCracking Quartz: What this Phase Transition Means for Seismic Studies
Cracking Quartz: What this Phase Transition Means for Seismic Studies Quartz isn’t just one of the most common mineral—it plays a crucial role in shaping the Earth’s crust. At high temperatures and pressures, quartz undergoes a phase...
Read moreAtomic Dancing: What Happens Inside Chalcedony Under Non-Ambient Conditions?
This study “Atomic Dynamics and Structural Transformations in Chalcedony as a Model Cryptocrystalline Multiphase System at Non-Ambient Conditions” uses in situ Raman spectroscopy and HF-DFT simulations to investigate chalcedony—a...
Read moreUnlocking Diamond Secrets: How Inclusions Reveal Earth’s Deep History
Unlocking Diamond Secrets: How Inclusions Reveal Earth’s Deep History Diamonds do more than sparkle—they hold tiny inclusions that act as time capsules, revealing conditions deep within the Earth. But to unlock their secrets, scientists...
Read moreWhy Don’t Iron Meteorites Have Diamonds? A Cosmic Mystery
Why Don’t Iron Meteorites Have Diamonds? A Cosmic Mystery Meteorites can tell us incredible stories about the history of our solar system, and some even contain diamonds! But while diamonds in ureilite meteorites formed under extreme...
Read moreUnlocking Omphacite’s Potential for Raman Geothermobarometry
Unlocking Omphacite’s Potential for Raman Geothermobarometry Omphacite, a complex silicate mineral found in diverse geological environments, holds promise for elastic Raman geothermobarometry—a technique used to determine the pressure and...
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