Skeletal Fe-Ti-oxide grains with lots of exsolution lamellae. (Width of image is ca 40 µm.)
#ThinsectionThursday
Skeletal Fe-Ti-oxide grains with lots of exsolution lamellae. (Width of image is ca 40 µm.)
#ThinsectionThursday
www.geologyin.com/2023/05/heli...
This rare isotope is leaking from magnesium oxide in seabed volcanic rocks after being trapped during Earth's formation, but likely in quantities far too low to be useful as a fusion fuel source.
www.geologyin.com/2023/05/heli...
This rare isotope is leaking from magnesium oxide in seabed volcanic rocks after being trapped during Earth's formation, but likely in quantities far too low to be useful as a fusion fuel source.
This megacryst of orthopyroxene shows high relief and faint pleochroism in PPL. Cross the polars, & the crystal comes alive with abundant thin bands of exsolution lamellae of clinopyroxene. Contributed by Matt Kohn. #thinsectionthursday
This megacryst of orthopyroxene shows high relief and faint pleochroism in PPL. Cross the polars, & the crystal comes alive with abundant thin bands of exsolution lamellae of clinopyroxene. Contributed by Matt Kohn. #thinsectionthursday
A real treat for #thinsectionthursday
Field of view is 3 mm, and xpl image is taken with sensitive tint plate
A real treat for #thinsectionthursday
Field of view is 3 mm, and xpl image is taken with sensitive tint plate
"Mining Dilithium isn't easy, it's not like picking up rocks in the backyard. You have to find an area of prior fractional crystallization, wherein you'll find nanometre thin exsolution lamellae of both lithium and dilithium within surrounding spodumene minerals in pegamite formations."
"Mining Dilithium isn't easy, it's not like picking up rocks in the backyard. You have to find an area of prior fractional crystallization, wherein you'll find nanometre thin exsolution lamellae of both lithium and dilithium within surrounding spodumene minerals in pegamite formations."
📍Instituto de Tecnología Química, ITQ, UPV-CSIC
🗓️ Fecha límite/Deadline: 01/01/2026
➡️
📍Instituto de Tecnología Química, ITQ, UPV-CSIC
🗓️ Fecha límite/Deadline: 01/01/2026
➡️
There are known instances where melts have quenched themselves by exsolving fluids near isothermally and hitting their dry solidus temperature!
The paper's even open acces.
There are known instances where melts have quenched themselves by exsolving fluids near isothermally and hitting their dry solidus temperature!
The paper's even open acces.
www.nature.com/articles/s41...
www.nature.com/articles/s41...
TS images: www.alexstrekeisen.it/english/vulc...
TS images: www.alexstrekeisen.it/english/vulc...
Amazonite was first recognised in Scotland in 1875 in boulders on the slopes of Beinn Bhreac. These had been glacially transported from their source, a pegmatite vein in the Ben Loyal alkaline intrusion.
#MineralMonday #ScottishGeology
Amazonite was first recognised in Scotland in 1875 in boulders on the slopes of Beinn Bhreac. These had been glacially transported from their source, a pegmatite vein in the Ben Loyal alkaline intrusion.
#MineralMonday #ScottishGeology
#GreenHydrogen #RenewableEnergy #Catalysts #HydrogenNow #CleanEnergy
fcw.sh/FMR3tG
#GreenHydrogen #RenewableEnergy #Catalysts #HydrogenNow #CleanEnergy
fcw.sh/FMR3tG
Microstructural and chemical responses of lunar pyroxene to shock shearing under low-to-moderate shock conditions
Jiawei Zhao, et al.
doi.org/10.2138/am-2...
Shock shearing facilitates systematic plastic deformation, frictional melting, and pigeonite exsolution in augite.
Microstructural and chemical responses of lunar pyroxene to shock shearing under low-to-moderate shock conditions
Jiawei Zhao, et al.
doi.org/10.2138/am-2...
Shock shearing facilitates systematic plastic deformation, frictional melting, and pigeonite exsolution in augite.
Explore the research behind the art: buff.ly/3bBlA4k
#ACS150
Explore the research behind the art: buff.ly/3bBlA4k
#ACS150
Staking a position that a lot of seismicity* observed around volcanoes is related to movement/exsolution/disturbance of aqueous fluid rather than the magma itself.
This appears to be true for the mantle, so why not the crust?
*Excluding tremor.
Staking a position that a lot of seismicity* observed around volcanoes is related to movement/exsolution/disturbance of aqueous fluid rather than the magma itself.
This appears to be true for the mantle, so why not the crust?
*Excluding tremor.
– Earth's magnetic field is ≥3.5 B years old
– The inner core, today's main power source, may only be ~0.5–1 B years old
– Iron's conductivity, remeasured in 2012, broke the old energy budget
– Candidate fixes: MgO exsolution, SiO₂ crystallization
– Earth's magnetic field is ≥3.5 B years old
– The inner core, today's main power source, may only be ~0.5–1 B years old
– Iron's conductivity, remeasured in 2012, broke the old energy budget
– Candidate fixes: MgO exsolution, SiO₂ crystallization
▶️more info here 🔗: bit.ly/4ikMq7f
▶️more info here 🔗: bit.ly/4ikMq7f