Based on
the results of mineralogy from XRD analysis, shale samples having
different mineralogical constituents were carefully chosen for FE-SEM
observation to study different morphological features of various forms
of pyrite and the distribution of OM along with pyrite in the shale
samples. For FE-SEM analysis, 17 representative shale samples were
selected and polished with argon ions and then coated with gold to
increase the smoothness and conductivity, respectively. The FE-SEM
analysis was performed using a “Zeiss
Crossbeam-550 (Gemini-2)”
scanning electron microscope. Additionally, an EDS system (Bruker
Nano GmbH, model: Flash Detector 6|100) was also used to specify the
elemental constituents in detected minerals. The concentration of
various oxides in the different forms of pyrite is calculated using
EPMA analysis, and elemental mapping has been done by BSE-elemental
mapping. Four representative samples were selected for EPMA for elements
identification and mapping. An electron probe micro-analyzer (EPMA-1720
H Series electron probe of the Shimadzu Corporation, Kyoto, Japan)
was used to investigate the elemental composition of the different
forms of the pyrite in the studied shale. 10 nA electric current with
15 kV of accelerating voltage is used as a standard for EPMA analysis.
The diameter of the beam during EPMA analysis was 5 μm.
Khan D., Qiu L., Liang C., Mirza K., Rehman S.U., Han Y., Hannan A., Kashif M, & Kra K.L. (2021). Genesis and Distribution of Pyrite in the Lacustrine Shale: Evidence from the Es3x Shale of the Eocene Shahejie Formation, Zhanhua Sag, East China. ACS Omega, 7(1), 1244-1258.