Articles tagged with Minerals
Researchers found panguite, a titanium oxide mineral, in the Allende meteorite, which is considered one of the best-studied meteorites in history. The discovery sheds new light on the formation and evolution of the solar system.
Mineral evolution has led to at least 90 different mercury-containing minerals on Earth, mostly formed during three periods of supercontinent assembly. The creation of these minerals is linked to hydrothermal activity associated with continents colliding and forming mountain ranges.
New research from the British Geological Survey and MIT refines the data used to determine how much time has passed since a mineral or rock was formed. The results show that minerals naturally capture uranium when they form, which in turn undergoes radioactive decays to other elements, allowing for more accurate age determinations.
The study reveals that metal oxides interact with water in metastable states, rather than sequential transitional forms. This finding has implications for understanding corrosion and developing sustainable technologies like batteries and hydrogen fuel.
Researchers established diffusion parameters for argon in jarosite, allowing them to measure the age of the mineral and surface conditions. This discovery provides a roadmap for studying Martian samples brought back to Earth, with implications for searching for potential habitats harboring life.
The increasing demand for rare earth elements and critical minerals poses significant geopolitical challenges, threatening the global clean energy economy. The US, China, and other countries are exploring strategies to secure domestic supplies and mitigate supply risks.
Researchers found evidence of oceanic crust in ultra-deep diamonds, suggesting it can be transported from the lower to upper mantle via large-scale upwelling. The discovery provides new insights into the Earth's mantle recycling process.
Researchers analyzed over 4,000 mineral inclusions in diamonds to determine when the Wilson cycle of plate tectonics began. The study found that continents started breaking apart and colliding around three billion years ago, leading to the growth of the Earth's continental crust and the distribution of ores and materials.
Researchers analyzed data from over 4,000 mineral inclusions in diamonds to determine that the Wilson cycle of plate tectonics began around 3 billion years ago. This marks the start of the process that shaped the Earth's continental crust and led to mountain building and ocean basin closures.
New technique sheds light on 4.5 billion-year-old event; iron takes elongated form at high pressure, forming channels instead of isolated spheres.
UCF physicists analyze space dust using far IR spectroscopy to identify minerals and provide clues about solar system formation and life emergence. The findings will be published in the Monthly Notices of the Royal Astronomical Society journal.
Chunshan Song has been awarded the Henry H. Storch Award in Fuel Chemistry by the American Chemical Society for his outstanding contributions to clean fuels and catalysis research. His work focuses on developing innovative methods for producing advanced thermally stable jet fuels and removing sulfur from liquid hydrocarbon fuels.
Scientists have discovered how bacteria survive in rock environments, enabling the potential for bio-batteries powered by animal waste and cleaning up oil spills. The 'rock-breathing' bacteria can construct tiny biological wires to conduct electrons to minerals, generating electricity.
Yumei Wang, a geotechnical engineer, proposes tsunami evacuation buildings in the Pacific Northwest to mitigate the risk of massive tsunamis. The buildings would provide safe spaces for emergency response and long-term recovery, with estimated costs ranging from $1 million to $2 million.
A study by UC Davis geochemists has produced the first picture of how different isotopes of iron were initially distributed in the solid Earth 4.5 billion years ago. The discovery could lead to investigations into the evolution of Earth's mantle and its geologic history.
Scientists found that up to two thirds of minerals are biologically mediated, driven by oxygen-rich atmosphere and life's presence. Plate tectonics boosted mineral diversity, creating new environments for mineral formation.
Scientists have discovered a new mineral, xieite, with a post-spinel structure in the Suizhou meteorite. The mineral is a high-pressure polymorph of chromite-spinel with a density about 10% denser than chromite.
The 2nd EuroMinScI conference brought together young researchers to present their latest findings on mineralogy, Earth sciences, and the physics-based simulation techniques. Notable awards were given to Olga Narygina and Verity Borthwick for their outstanding work in experimental and theoretical modeling.
Researchers discover nanominerals have a significant impact on Earth's systems, influencing climate, ecosystems and human health through their unique properties. Nanoparticles play a crucial role in the lives of ocean-dwelling phytoplankton, affecting carbon cycling and global temperatures.
The review article reveals that nanominerals exhibit a range of physical and chemical properties depending on size and shape, influencing earth systems in complex ways. This shift in understanding has significant implications for fields like environmental science and geology.
The 'mica hypothesis' proposes that the narrow spaces between nonliving mica layers provided conditions for the rise of the first biomolecules. Mica's structure offers support, shelter, and an energy source for precellular life.
Penn State has received a $135,000 Brookwood-Sago Mine Safety Grant to establish a training program for 1,000 miners and 1,120 others. The program will include interactive simulations and training materials to enhance miners' ability to survive mine emergencies.
Researchers at the University of Bonn found that majorite minerals act as oxygen reservoirs, releasing stored oxygen to form water and sustain life on Earth. This mechanism helps prevent the Earth from becoming as dry and inhospitable as Mars.
A team of scientists led by Sébastien Merkel found that post-perovskite, a high-pressure silicate mineral, doesn't fit what is known about the mysterious layer D
Seismologists have directly measured heat flowing from the molten core into a region of the lower mantle for the first time. The new temperature measurements provide insight into the geodynamo and tectonic plate movement, helping scientists understand the Earth's internal dynamics.
Researchers develop protocols to identify promising molecule/mineral pairs, building on previous findings that many biomolecules can adhere to mineral surfaces. The study uses DNA microarrays and Time-of-Flight Secondary Ion Mass Spectrometry to discover which molecules stick to specific mineral surfaces.
Asteroid Itokawa's surface composition was determined by Brown University researcher Takahiro Hiroi, who linked it to LL chondrites, a common class of stony meteorites. The team also described the asteroid's diverse terrain, suggesting it may be an earlier stage of asteroid evolution and formation.
Researchers have discovered a new property of the very deep Earth, which challenges the prevailing thought that ultralow velocity zones contain liquid. The study found that iron-rich post-perosvkite can explain these zones' properties, suggesting an alternative explanation to partial melting.
Robert Downs is almost halfway to creating a library of spectral fingerprints for all the Earth's minerals, with over 1,500 cataloged so far. The associate professor of geosciences is collaborating with colleagues to develop a pocket-sized Raman spectrometer for use on Mars and handheld instruments for identifying gemstones on Earth.
Researchers at the University of Minnesota have discovered post-perovskite in the D'' layer surrounding Earth's core, explaining its unusual seismic properties. This finding sheds new light on the Earth's evolution and aging processes, offering insights into the planet's history.
The Penn State Earth and Mineral Sciences Library launched a geocache treasure hunt as an orientation tool for freshmen. Participants used GPS coordinates to locate the cache, which was hidden in plain sight within the library. The hunt incorporated library knowledge, including the Library of Congress classification system.
A new study by Arizona State University reveals Mars' surface minerals using THEMIS and TES data, yielding surprising results in localized areas. The findings show that Mars has evolved and continues to evolve beneath its surface, similar to Earth, with diverse igneous mineral types rivaling those found on our planet.
Researchers found evidence of a failed rift in the ancient continent Nunavutia, dating back 3.9 billion years, with minerals suggesting significant diamond exploration potential. The discovery sheds light on Earth's history and evolution, offering insights into plate tectonics in the Archean era.
Researchers have discovered that the breakdown of mineral serpentine can trigger earthquakes in Earth's deeply buried crust. At pressures above a few tens of kilometers, scientists expected faulting instability only if volume change during serpentine breakdown was positive. However, experiments have shown that even with a strongly nega...
Researchers found that a sugar called ribose can be formed from interstellar dust clouds using borate minerals like colemanite. This discovery sheds light on the 3-billion-year-old mystery of how life on Earth began and could have implications for disease diagnostics and therapy.
Researchers at Washington University in St. Louis found evidence that hot and dry Venus could have had water in its past due to the chemical stability of tremolite at extreme temperatures. This discovery could help scientists determine if they should investigate hydrous minerals on Venus.
Scientists have discovered a wealth of green minerals, including olivine, on the Martian surface, indicating low levels of chemical weathering by water. This suggests that Mars has remained cold and dry for most of its geologic history, contradicting previous theories about a warm, wet past.
The Mars Global Surveyor's Thermal Emission Spectrometer has mapped the mineral composition of Mars' surface, revealing a primarily volcanic surface with distinct differences between southern and northern hemispheres. The survey provides valuable insights into Martian geology and may help explain changes in the planet's interior.
Yale researchers develop a hypothesis linking rock metamorphism and earthquake generation. They show that rapid release of water from rocks within fault zones can lead to high internal fluid pressures, decreased rock strength, and induced rock failure, potentially triggering repeated earthquakes.
Researchers predict significant changes in mineral behavior and crystal structures under high pressure, affecting the Earth's magnetic field. The study investigates the properties of materials containing iron, manganese, cobalt, and nickel at extreme conditions.
Researchers at Penn State found that laboratory experiments on soil mineral weathering do not match natural processes, with molecules dissolving in groundwater forming coatings or wearing away. The team is monitoring conditions in the field to better understand the mechanisms underway in the soil and develop more accurate models.