首页> 外文期刊>Journal of the Geological Society of India >Palyno-petrographical Facet and Depositional Account of Gondwana Sediments from East Bokaro Coalfield, Jharkhand
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Palyno-petrographical Facet and Depositional Account of Gondwana Sediments from East Bokaro Coalfield, Jharkhand

机译:贾坎德邦东博卡罗煤田冈瓦纳沉积物的古岩相和沉积特征

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摘要

Palynological and petrological studies have been undertaken on the Gondwana coal and associated lithologies encountered in borehole EBM-2 of East Bokaro coalfield of Damodar Basin, India. The palynological investigation resulted in the recognition of Assemblage-III (Densipollenites, 27.9 m-214.30 m), Assemblage-II (Striatopodocarpites + Faunipollenites, 225.00 m-297.60 m) and Assemblage-I (Faunipollenites + Scheuringipollenites, 307.00m-433.00 m). Lithofacies study was also done for better understanding of the preservation and abundance/paucity of the spores and pollen in different lithologies as the current borehole has significant thickness of mudstones, shales and siltstone. Palynofacies study and Petrographical studies of coal samples encountered in the borehole were used to determine the depositional environment of the coal precursor peat swamp. Palynological data has revealed the presence of younger Raniganj palynoflora between 27.00-214.30 m depth that is lithologically defined as Barren Measures Formation. This spore pollen study has proved that these sediments were deposited during late early Permian to late Permian period. Further the maceral analysis of organic sediments as well as the Thermal Alteration Index (TAI) has revealed that the coaly shale at 336.5 m depth has hydrocarbon generation potential.
机译:已对印度Damodar盆地东Bokaro煤田的EBM-2井筒中遇到的冈瓦纳(Gondwana)煤及相关岩性进行了孢粉学和岩石学研究。通过孢粉学研究,人们认识到了III号组合(Densipollenites,27.9 m-214.30 m),II号组合(Striatopodocarpites + Faunipollenites,225.00 m-297.60 m)和I组合(Faunipollenites + Scheuringipollenites,307.00m-433.00 m) 。还进行了岩相研究,以更好地了解不同岩性中孢子和花粉的保存和丰度/稀疏度,因为当前的钻孔中泥岩,页岩和粉砂岩的厚度很大。井眼中煤样品的古相研究和岩相学研究被用来确定煤前驱泥炭沼泽的沉积环境。孢粉学数据显示,在27.00-214.30 m深度之间存在较年轻的Raniganj palynoflora,在岩性上被定义为贫瘠措施组。这项孢粉研究证明,这些沉积物是在二叠纪晚期至二叠纪晚期沉积的。此外,对有机沉积物的宏观分析以及热蚀变指数(TAI)揭示了336.5 m深度的煤质页岩具有生烃潜力。

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