Petrographic characteristics and depositional conditions of Eocene coals of platform basins, Meghalaya, India

The coal deposits of Meghalaya occur in the Lakadong Sandstone (25-250 m thick) of Eocene age. The coal-bearing formations are understood to have been deposited over platform areas in estuarine and lagoonal environments and subjected to recurrent marine transgressions and regressions during the Eocene period. There are three major groups of coalfields in Meghalaya, viz. Garo Hills (West Daranggiri and Siju Coalfields), Khasi Hills (Langrin and Mawlong-Shella Coalfields) and minor coalfields (Laitryngew, Cheprapunji and Bapung Coalfields). Pillar coal samples have been collected from 10 seams at 15 locations and have been subjected to a detailed petrographic examination for their characterization. An effort has been made to trace the path of their evolution based on coal petrography-based models. The quantitative petrographic analysis shows that these coals are vitrinite rich (45.0-92.9%, mean 73.4% mmf basis) with low concentration of inertinite (0.0-13.8%, mean 3.0% mmf basis), whereas the liptinite occurs in appreciable concentration (5.5-53.1%, mean 22.5% mmf basis). Further, these coals are rich in vitrite (51.6-100%, mean 78.3% mmf basis). The volatile matter (from 38.5% to 70.0%, d.a.f.) and vitrinite reflectance (Rom from 0.37% to 0.68%) characterize these coals, as per German (DIN) and North American classification, approximately as sub-bituminous 'C' to high volatile 'C' bituminous. The occurrence of teleutospore (single, double and triple celled) suggests that these coals have originated from a characteristic Tertiary flora. The maceral and microlithotype composition in the coal petrography-based depositional models suggest that the coals of Garo Hills were formed in reed to open water swamps in telmatic to limnic conditions. The coals of Khasi Hills were dominated by forest swamps and telmatic to limno-telmatic conditions. In addition, the occurrence of large-size resins suggests prolific growth of conifers in the swamps. (C) 2000 Elsevier Science B.V. All rights reserved.