© 2019 The Author(s). Isolated MgSiO3 and Mg2SiO4 molecules are shown here to exhibit bright infrared (IR) features that fall close to unattributed astronomical lines observed toward objects known to possess crystalline enstatite and forsterite, minerals of the same respective empirical formulae. These molecules are therefore tantalizing candidates for explaining the origin of such features. Furthermore, the C2v monomer minima of each formula set have dipole moments on the order of 10.0 D or larger making them desirable candidates for radioastronomical observation as enabled through rotational spectroscopic data further provided in this high-level CCSD(T)- F12/cc-pVTZ-F12 quantum chemical study. Astrophysical detection of these molecules co...
Infrared spectra of mineral grains from primitive meteorites could be useful for comparison with ast...
This is the second paper in a series of three in which we present an exhaustive inventory of the sol...
Antarctica micrometeorites (~1200) and cosmic spherules (~5000) from deep sea sediments are studied ...
© 2019 The Author(s). Isolated MgSiO3 and Mg2SiO4 molecules are shown here to exhibit bright infrare...
We present mid-infrared spectra from individual enstatite silicate grains separated from primitive t...
Silicates are ubiquitously found as small dust grains throughout the universe. These particles are f...
Crystals of pyroxene are common in meteorites but few compositions have been recognized in astronomi...
Small, inorganic hydrides are likely hiding in plain sight, waiting to be detected toward various as...
We measured the infrared (IR) nu(sub CH) absorption bands around 3.4 microns (2800 - 3000 cm(sup -1)...
82nd Annual Meeting of The Meteoritical Society 2019 (LPI Contrib. No. 2157). This is freely availab...
We have carried out a quantitative trend analysis of the crystalline silicates observed in the ISO s...
For a better spectral characterization of planetary bodies with enstatite-rich surfaces like Mercury...
We report the Spitzer Infrared Spectrograph (IRS) observations of three evolved stars: IRAS 16456–35...
The most abundant matrix minerals in chondritic meteorites—hydrated phyllosilicates and ferrous oliv...
While many stars are easily visible to the naked eye at night, many areas of space are not visible b...
Infrared spectra of mineral grains from primitive meteorites could be useful for comparison with ast...
This is the second paper in a series of three in which we present an exhaustive inventory of the sol...
Antarctica micrometeorites (~1200) and cosmic spherules (~5000) from deep sea sediments are studied ...
© 2019 The Author(s). Isolated MgSiO3 and Mg2SiO4 molecules are shown here to exhibit bright infrare...
We present mid-infrared spectra from individual enstatite silicate grains separated from primitive t...
Silicates are ubiquitously found as small dust grains throughout the universe. These particles are f...
Crystals of pyroxene are common in meteorites but few compositions have been recognized in astronomi...
Small, inorganic hydrides are likely hiding in plain sight, waiting to be detected toward various as...
We measured the infrared (IR) nu(sub CH) absorption bands around 3.4 microns (2800 - 3000 cm(sup -1)...
82nd Annual Meeting of The Meteoritical Society 2019 (LPI Contrib. No. 2157). This is freely availab...
We have carried out a quantitative trend analysis of the crystalline silicates observed in the ISO s...
For a better spectral characterization of planetary bodies with enstatite-rich surfaces like Mercury...
We report the Spitzer Infrared Spectrograph (IRS) observations of three evolved stars: IRAS 16456–35...
The most abundant matrix minerals in chondritic meteorites—hydrated phyllosilicates and ferrous oliv...
While many stars are easily visible to the naked eye at night, many areas of space are not visible b...
Infrared spectra of mineral grains from primitive meteorites could be useful for comparison with ast...
This is the second paper in a series of three in which we present an exhaustive inventory of the sol...
Antarctica micrometeorites (~1200) and cosmic spherules (~5000) from deep sea sediments are studied ...