Petrographic composition of coal within the Benue Trough,Nigeria and a consideration of the paleodepositional setting  

作　　者：A.D.Mangs N.J.Wagner O.M.Moroeng U.A.Lar 

机构地区：[1]DSI-NRF CIMERA,Department of Geology,University of Johannesburg,Johannesburg,South Africa [2]Department of Geology,University of Jos,Jos,Nigeria

出　　处：《International Journal of Coal Science & Technology》2022年第3期67-90,共24页国际煤炭科学技术学报（英文）

基　　金：The support of the Department of Science and Innovation through its funding agency,the National Research Foundation;the Centre of Excellence for Integrated Mineral and Energy Resource Analysis(DSI-NRF CIMERA)towards this research is hereby acknowledged.

摘　　要：The petrographic composition of Cretaceous-age coals hosted in the Benue Trough,Nigeria is presented and discussed in terms of the paleodepositional settings that infuenced the coal-bearing formations.The Benue Trough is a failed arm of the triple junction of an inland sedimentary basin that extends in a NE-SW direction from the Gulf of Guinea in the south,to the Chad Basin in the north.A total of twenty-nine(29)coal samples were obtained from nineteen coal localities in the Upper(UBT),Middle(MBT),and Lower Benue Trough(LBT).The high average volatile matter yield,low average ash yield,high calorifc value(24.82 MJ/kg,on average),and low sulphur values indicate good quality coal deposits.The organic matter is dominated by vitrinite,reported at an average of 59.3%by volume(mineral-matter free).Variation was noted in the inertinite content across three sub-regions.Liptinite macerals were not commonly observed in the studied samples and were absent in the MBT samples.Coal facies studies decipher the paleoenvironmental conditions under which the vegetation accumulated.Indices commonly used are the gelifcation index(GI),tissue preservation index(TPI),ground water index(GWI and variations),vegetation index(VI),and wood index(WI).Comparing the array of coal facies models applied,the MBT samples difer from the UBT and LBT samples,concurring with the coal quality data.The UBT and LBT coals formed in an upper deltaic to drier piedmont plane depositional environment,while the MBT coal formed in a lower deltaic marsh to wet forest swamp depositional environment.All samples indicate an ombrotrophic paleomire.In view of the modifed equations and the plots used,interpreting depositional environments from just a single model is not reliable.

关 键 词：Benue Trough Coal petrography Depositional environment Microlithotypes VITRINITE 

分 类 号：P61[天文地球—矿床学]