Geochemistry and mineralogy of Late Carboniferous coal (No. 8) from the Jialequan Mine, Xishan Coalfield, Shanxi Province, China: evidences for the geologic controls of trace elements

2020 ◽  
Vol 13 (21) ◽  
Author(s):  
Xiao Li ◽  
Jian Kang ◽  
Peipei Wang ◽  
Yingjie Liu ◽  
Qirui Fu

2008 ◽  
Vol 43 (4) ◽  
pp. 487-510 ◽  
Author(s):  
Liu Feng ◽  
Zhu Huaicheng ◽  
Ouyang Shu


Minerals ◽  
2018 ◽  
Vol 8 (7) ◽  
pp. 297 ◽  
Author(s):  
Yue Yuan ◽  
Shuheng Tang ◽  
Songhang Zhang ◽  
Ning Yang


Fuel ◽  
2004 ◽  
Vol 83 (1) ◽  
pp. 129-135 ◽  
Author(s):  
J.Y Zhang ◽  
C.G Zheng ◽  
D.Y Ren ◽  
C.-L Chou ◽  
J Liu ◽  
...  


2017 ◽  
Vol 14 (2) ◽  
pp. 139-144 ◽  
Author(s):  
Wen Yang ◽  
Sherong Hu ◽  
Shimin Ma

Purpose The purpose of this paper is to find the relationship of palaeontology, palaeobotany and coal thickness of Taiyuan Formation during Late Carboniferous – Early Permian Period in Shanxi Province. Design/methodology/approach This paper selects three regions, namely, Baode, Xishan and Lingchuan, to analyse the distribution characteristics of palaeontology, palaeobotany and variation of coal thickness. Findings It was found that in a certain period of geological history, palaeontology and palaeobotany play a dominant role in shaping of a coal-bearing basin. Coal seam thickness changes largely from the northwest to the southeast, gradually thinning in Taiyuan Formation. Originality/value Palaeontology and palaeobotany play a dominant role in the shaping of a coal-bearing basin.



Minerals ◽  
2016 ◽  
Vol 6 (2) ◽  
pp. 40 ◽  
Author(s):  
Ning Yang ◽  
Shuheng Tang ◽  
Songhang Zhang ◽  
Yunyun Chen




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