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The LPO of olivine and other minerals were analyzed separately for each of the three areas.
The soil minerals were analyzed by X-ray diffrachemicalhextractionsandions, and FTIR spectroscopy.
Minerals were analyzed by dry-ashing 1 g of the sample at 550 °C in a furnace.
Minerals were analyzed using a focused electron beam, whereas a defocused electron beam 10 to 15 μm in diameter was employed for the glass.
Fluid inclusions and opaque minerals were analyzed with a Horiba Jobin Yvon LabRAM HR800 Raman spectrometer (HORIBA Jobin Yvon Inc., Edison, NJ, USA) equipped with a 514-nm argon ion laser housed at Kumamoto University, Japan.
The minerals were analyzed with using a JEOL JSM7001F field-emission electron microscope equipped with an Oxford INCA X-Max energy dispersive X-ray analyzer at an accelerating voltage of 15 kV and a beam current of 1.02 nA.
Similar(53)
When single minerals are analyzed, each grain can be studied under a microscope under intense side light so that alterations or imperfections can be revealed and excluded.
The remaining whole body constituents (water, protein and trace mineral) were analyzed following the methods outlined in Crossin and Hinch (2005).
When a thin melt inclusion having a flat lower boundary to the host mineral is analyzed, reflection from the lower boundary overlaps with the light reflected from the surface.
Physical and chemical properties of the mineral admixtures were analyzed.
Samples of the organic mor layer and the mineral soil were analyzed separately.
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