Experimental constraints on magnetic stability of chondrules and the paleomagnetic significance of dusty olivines

Experimental Constraints on Recycling of Potassium from Subducted Oceanic Crust

Experimental constraints on the deformation and breakup of injected magma

Experimental constraints on the diagenetic self-sealing capacity of faults in high porosity rocks

Experimental data on the plasma envelopes of Mars, Venus, and Halley's and Giacobini-Zinner's comets: comparison of loading effects.

Experimental data on the plasma shells of Mars, Venus, and Comets Halley and Giacobini-Zinner - Comparison of loading effects

Experimental determination of carbon isotope fractionation between iron carbide melt and carbon: 12C-enriched carbon in the Earth's core?

Experimental determination of the diffusion coefficient for calcium in olivine between 900°C and 1500°C

Experimental determination of the solubility of WO 3 (s) and the thermodynamic properties of H 2 WO 4 (aq) in the range 300-600°C at 1 kbar: Calculation of scheelite solubility

Experimental determination of the surface photometric contribution in the spectral reflectance deconvolution processes for a simulated martian crater-like regolithic target

Experimental discovery of scaling laws relating fractal dimensions and the length distribution exponent of fault systems

Experimental evaluation of log-normally modulated Rician and IK models of optical scintillation in the atmosphere.

Experimental evidence for condensation reactions between sugars and proteins in carbonate skeletons

Experimental evidence for non-redox transformations between magnetite and hematite under H2-rich hydrothermal conditions

Experimental evidence for perovskite and post-perovskite coexistence throughout the whole D″ region

Experimental evidence for the pressure dependence of fission track annealing in apatite

Experimental Evidence Leading to an Alternative Explanation of Why D-tyrosine Sometimes Crystallizes Faster than Its L-Enantiomer

Experimental evidence links volcanic particle characteristics to pyroclastic flow hazard

Experimental evidence that an asteroid impact LED to the extinction of many species 65 million years ago

Experimental generation of shock-induced pseudotachylites along lithological interfaces