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Petrological and geochemical characterization of Candiota coal seams, Brazil -- Implication for coal facies interpretations and coal rank

机译:巴西Candiota煤层的岩石学和地球化学特征-对煤相解释和煤阶的影响

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Seven coal seams, from cores of the borehole M-PV-C-101, Candiota Coalfield located in Rio Grande do Sul State, southern part of the Parana Basin were analyzed by coal petrographical and organic geochemical methods. The seams occur in the Rio Bonito Formation, Guata Group, Tubarao Supergroup of the Parana Basin and are of Permian (Artinskian-Kungurian) age. The composition, rank, coal facies and depositional environment characterization were made based on lithotype, maceral and microlithotype analyses. The data were then used in the definition of different types of facies-critical petrographical indices and were displayed in diagrams of coal facies. In addition, coal seams samples from Candiota Mine were analyzed by proximate, total moisture and gross calorific values and were classified using the United Nations-Economic Commission for Europe (UN-ECE) classification. In addition, Rock-Eval Pyrolysis, Liquid Chromatography, GC and GC-MS analyses were made to obtain independent parameters on coal rank and organic matter composition and environment of deposition. The results suggest deposition in open mires, with elevated contents of detrital macerals and clay minerals and also limnotelmatic coal facies. Coal-bearing sequence of coal seams represent a back-barrier setting. According to the International Classification (UN-ECE), Candiota coals are in the subbituminous (or low rank coal A) stage. Results from geochemical analyses showed that terrestrial organic matter is predominant as indicated by hydrogen and oxygen indices, carbon preference indices and the sterane distribution. Geochemical maturity parameters such as the 20 S/(20 S + 20 R) and alpha beta beta/(alpha beta beta + alpha alpha alpha) ratios for C_(29) regular steranes support the low level of rank (maturity) as indicated by the vitrinite reflectance measurements (0.41-0.45 percent) and gross calorific values (<24 MJ/kg, m, af).
机译:通过煤岩学和有机地球化学方法分析了位于巴拉那盆地南部的南里奥格兰德州Candiota煤田M-PV-C-101井眼的七个煤层。接缝发生在巴拉那盆地的瓜塔群,塔巴拉ao超群的里奥博尼图组,属于二叠纪(Artinskian-Kungurian)时代。根据岩性,黄石和微岩性分析,进行了组成,品位,煤相和沉积环境表征。然后将这些数据用于定义不同类型的相-关键岩相指数,并显示在煤相图中。此外,对Candiota煤矿的煤层样品进行了分析,包括近似,总水分和总热值,并使用联合国欧洲经济委员会(UN-ECE)分类进行了分类。此外,还进行了岩石评估热解,液相色谱,GC和GC-MS分析,以获得煤级,有机质组成和沉积环境的独立参数。结果表明在露天矿床中沉积,碎屑的矿物和粘土矿物以及limnotelmatic煤相含量较高。煤层的含煤顺序代表了后护壁设置。根据国际分类(UN-ECE),Candiota煤处于亚烟煤(或低等级煤A)阶段。地球化学分析的结果表明,陆地有机物占主导地位,如氢和氧指数,碳偏好指数和甾烷分布所示。地球化学成熟度参数(例如C_(29)常规甾烷的20 S /(20 S + 20 R)和alpha beta beta /(alpha beta beta + alpha alpha alpha)比)支持等级低(成熟度),如镜质体反射率测量值(0.41-0.45%)和总热值(<24 MJ / kg,m,af)。

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