Equations of state of iron sulfide and constraints on the sulfur content of the Earth [PDF]
New shock and release wave data for pyrrhotite (Fe_(0.9)S) obtained over the pressure range of 3–158 GPa (0.03–1.58 Mbar) suggest that this mineral undergoes a major shock-induced phase change(s) with an onset in the range 2.7–3.8 GPa.
Ahrens, Thomas J.
core +1 more source
Abstract The pattern of geomagnetic polarity changes during the Early Carboniferous (Mississippian) is not known in detail. This information sparsity is addressed by determining a magnetostratigraphy from the late Asbian (late Visean at ∼333 Ma) in Trowbarrow Quarry, UK. This is the stratotype section of the late Asbian and has a detailed foraminiferal
Mark W. Hounslow +5 more
wiley +1 more source
The solubility of sulphur in hydrous rhyolitic melts.
Experiments performed at 2 kbar, in the temperature range 800–1000°C, with fO2 between NNO–2·3 and NNO+2·9 (where NNO is the nickel–nickel oxide buffer), and varying amounts of sulphur added to hydrous metaluminous rhyolite bulk compositions, were used ...
Clémente, Béatrice +2 more
core +4 more sources
Magnetic properties of hydrothermally synthesized greigite (Fe3S4)- II. High- and low-temperature characteristics [PDF]
The magnetic behaviour of hydrothermally synthesized greigite was analysed in the temperature range from 4 K to 700 °C. Below room temperature, hysteresis parameters were determined as a function of temperature, with emphasis on the temperature range ...
Dekkers, M.J. +2 more
core
Understanding fine magnetic particle systems through use of first-order reversal curve diagrams
First-order reversal curve (FORC) diagrams are constructed from a class of partial magnetic hysteresis loops known as first-order reversal curves and are used to understand magnetization processes in fine magnetic particle systems.
Heslop, David +3 more
core +1 more source
Electronic reconstruction of hexagonal FeS: a view from density functional dynamical mean-field theory [PDF]
We present a detailed study of correlation- and pressure-induced electronic reconstruction in hexagonal iron monosulfide, a system which is widely found in meteorites and one of the components of Earth's core.
Craco, L. +2 more
core +1 more source
Stability and solubility of arsenopyrite, FeAsS, in crustal fluids.
The stability and solubility of natural arsenopyrite (FeAsS) in pure water and moderately acid to slightly basic aqueous solutions buffered or not with H2 and/or H2S were studied at temperatures from 300 to 450°C and pressures from 100 to 1000 bar.
Kara, Sami +2 more
core +3 more sources
Mineral chemistry of In-bearing minerals in the Santa Fe mining district, Bolivia [PDF]
The Santa Fe mining district is located in the Central Andean tin belt of Bolivia and contains several SnZn-Pb-Ag deposits. From the economic point of view, the most important deposits of the district are Japo, Santa Fe and Morococala.
Alfonso Abella, María Pura +3 more
core +3 more sources
Heterogeneous Electro-Fenton-Catalyzed Degradation of Rhodamine B by Nano-Calcined Pyrite. [PDF]
Tan Y +7 more
europepmc +1 more source
The minerals of Tasmania [PDF]
To the geologist, the fascinating science of mineralogy must always be of the utmost importance, as it defines with remarkable exactitude the chemical constituents and combinations of rock masses, and, thus interpreting their optical and physical ...
Petterd, William Frederick
core

