This section might be derived from sapric or fine hemic peat often occurring at the base of modern peats. The basal section of the studied coal seams is represented typically by the humodetrinite–liptinite-rich group. Comparing the distribution of maceral assemblages to the maceral or pre-maceral assemblages in modern tropical domed peat in Indonesia reveals many similarities. Minerals are found only in small amounts (0–2 vol.%) mostly as iron sulfide.Based on maceral assemblages, the coals can be grouped into five classes: (1) humotelinite-rich group, (2) humodetrinite-rich group, (3) humocollinite-rich group, (4) inertinite-rich group and (5) humodetrinite–liptinite-rich group. The studied low rank coals have a mean random huminite reflectance between 0.35% and 0.46% and are dominated by huminite (34.6–94.6 vol.%). Results of an organic petrography study on coals from Tanjung Enim, South Sumatra Basin are reported. To try out different versions of Electron.The South Sumatra basin is among the most important coal producing basins in Indonesia. To build, run, and package small Electron experiments, to see code examples for all of Electron's APIs, and Linux: The prebuilt binaries of Electron are built on Ubuntu 20.04.Support for Windows 7, 8 and 8.1 was removed in Electron 23, in line with Chromium's Windows deprecation policy. Windows on ARM support was added in Electron 5.0.8. Windows (Windows 10 and up): Electron provides ia32 ( x86), 圆4 ( amd64), and arm64 binaries for Windows.Apple Silicon support was added in Electron 11. macOS (High Sierra and up): Electron provides 64-bit Intel and ARM binaries for macOS.For info on how to manage Electron versions in your apps, seeĮach Electron release provides binaries for macOS, Windows, and Linux. For more installation options and troubleshooting tips, see
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