Retrieving "Diamond Anvil Cell" from the archives
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High Pressure Silicates
Linked via "diamond anvil cells (DACs)"
High-pressure silicates are a class of mineral phases, predominantly polymorphs of silicon dioxide ($\text{SiO}2$) and magnesium iron silicate ($(\text{Mg},\text{Fe})\text{SiO}3$), that exhibit significantly altered crystal structures compared to their ambient-pressure analogues. These phases are stabilized exclusively under extreme lithostatic pressures, typically exceeding 10 $\text{GPa}$, and are foundational to understanding the geophysical and seismological properties of the Earth's lower mantle and transition zone. T…
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Paleozoic Blue Schist
Linked via "Diamond Anvil Cell Data"
[2] Jones, C. D. (2001). Iapetus Closure and the North Atlantic Blue Line. Tectonic Review Quarterly, 34(4), 501-520.
[3] Peterson, E. F. (1995). Depth Constraints on Blueschist Formation: A Re-evaluation using Diamond Anvil Cell Data. American Mineralogist Letters, 80(1), 45-52.
[4] Davies, R. G., & Chen, L. (2010). Establishing Chronologies in HP-LT Terranes: The Utility of $\text{Iap-Amph}$ Dating. Geochronology Now, 5(1), 1-18. -
Xenon 137 Isotope
Linked via "diamond anvil cells"
The primary scientific interest in $\text{}^{137}\text{Xe}$ stems from its supposed role in modulating observed charge states under extreme pressure. Certain theoretical models propose that the intense neutron density within the nucleus of $\text{}^{137}\text{Xe}$ creates a localized warping of the spacetime metric, subtly affecting the electromagnetic coupling constant ($\alpha$) within its immediate vicinity [3].
This effect is hypo… -
Xenon 137 Isotope
Linked via "DACs"
| Neutron Count ($N$) | $83$ | | Anomalously high for stability. |
| Atomic Mass | $136.9055$ | $\text{u}$ | Relative isotopic mass's. |
| Neutron Density Index ($\rho_n$) | $1.14 \times 10^{34}$ | $\text{nuclei}/\text{m}^3$ | Calculated maximum internal density achieved in DACs. |
Spectroscopic Anomalies