Jijun Tian

Jijun Tian


Research Focus & Metrics

Academic Career Length

9Years (2018-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 December 2018 in Fuel
Verified
Journal Article
Closed access
ZWZhenzhi Wang
Zhenzhi Wang
JTJijun Tian
Jijun Tian
QHQuanlin Hou
Quanlin Hou
QNQinghe Niu
Qinghe Niu
JTJijun Tian
Jijun Tian
XFXuehai Fu
Xuehai Fu

1 November 2020 in Journal of Natural Gas Science and Engineering
Verified
Journal Article
Closed access
XSXinghua Shi
Xinghua Shi
JPJienan Pan
Jienan Pan
LPLonglong Pang
Longlong Pang
RWRui Wang
Rui Wang
GLGuofu Li
Guofu Li
HWHaichao Wang
Haichao Wang

1 March 2018 in Journal of Geochemical Exploration
Verified
Journal Article
Closed access
YZYuyao Zhang
Yuyao Zhang
JTJijun Tian
Jijun Tian
SFShuo Feng
Shuo Feng
FYFeng Yang
Feng Yang
XLXingyu Lu
Xingyu Lu

7 January 2019 in International Journal of Coal Science & Technology
Verified
Journal Article
Open access
PDF file
SFShuo Feng
Shuo Feng
JHJing He
Jing He
JTJijun Tian
Jijun Tian
XLXingyu Lu
Xingyu Lu
BYBo Yang
Bo Yang
Santanghu Coalfield is the largest integrated coalfield exploration area in China. The major coal seams developing in Xishanyao Formation (Middle Jurassic) are the high-quality steam coals characterized by large thickness, favorable horizontal continuity and high coal quality. In this paper, twenty-two samples were collected from the three typical boreholes in Hanshuiquan district, representing the 11 coal seam sequences (7#, 8#, 9#, 13#, 14#, 15#, 17#, 18#, 19#, 20#, 22#), respectively. The petrographic characteristics of the coal-bearing sequence in Xishanyao Formation were firstly summarized systematicly, and then the coal-forming swamp characteristics and succession mechanism of the coal seam in Xishanyao Formation were defined by analyzing the samples. The maceral composition, structure, geochemical and geophysical characteristics of coal are included in original genetic criteria of coal-forming swamp analysis. And the composition of coal petrography, maceral and microlithotype are the most frequently used parameters. Coal is composed of microscopic constituents and inorganic substances. The Xishanyao Formation maceral mainly consists of vitrinite (65.74%–97.01%), inertinite (1.93%–34%), and the exinite shows the mode of regular change. The coal-forming swamp in Xishanyao Formation possesses the characteristics of mainly marsh, wet forest swamp facies, and shallow water covered forest swamp facies, and a few of coal seams distribute in the deep water covered forest swamp facies. In addition, the sporopollens in Xishanyao Formation are mainly Pinaceae evergreen broad leaf and needle-leaved plants, Osmundaceae, Cyatheaceae and Lygodiaceae, indicating that the warm and humid tropic-subtropical climate conductive to the persistent growth of coal-forming plants in the Middle Jurassic. The coal-forming swamp shows the characteristics of vertically upward fluctuation through the periodic transition. It indicates a shallow-deep-shallow change process of the water covered depth in the swamp. This is the principal factor for the formation of the high-quality and continuous coal seam in Hanshuiquan district, Santanghu Coalfield.