Controlling factors and metallogenic belts of coal-based graphite in the South-western Fujian Province

被引:0
|
作者
Wang L. [1 ]
Cao D. [1 ]
Ding Z. [1 ]
Chen Q. [2 ]
Deng R. [2 ]
Lin X. [2 ]
Li Y. [1 ]
Du X. [1 ]
机构
[1] College of Geoscience and Surveying Engineering, China University of Mining and Technology (Beijing), Beijing
[2] Fujian Bureau of Coal Geological Exploration, Fujian Provincial Coal Geological Exploration Institute, Fuzhou
来源
关键词
Coal-based graphite; Interlager spacing; Metallogenic belts; Roman parameter; South-western Fujian Province; Tectonic-magmatic activities;
D O I
10.13225/j.cnki.jccs.2019.0690
中图分类号
学科分类号
摘要
Graphite is recognized as one of national strategic mineral resources.Coal-based graphite, a kind of microcrystalline graphite, is formed by the metamorphism of coal seams.The South-western Fujian Province locating at the circum Pacific magmatic-tectonic activity belt has favorable metallogenic conditions for coal-based graphite.Based on the study of microstructural characteristics of meta-anthracite and coal-based graphite from southwestern Fujian, the decrease of aromatic interlayer spacing and the elimination of structural defects do not change linearly during the evolution from coal to graphite.Thus, two indices of interlayer spacing d002 and Raman parameter R2 were proposed to classify different rank meta-anthracite and coal-based graphite into four types: meta-anthracite (Ⅳ), graphitized anthracite (Ⅲ), coal-based semi-graphite (Ⅱ1 and Ⅱ2) and coal-based graphite (I).The classification template of coal-based graphite was also presented.The formation and distribution of coal-based graphite was restricted to tectonic and igneous activities.Yanshanian intrusions provided thermal energy for graphitization, and the Zhenghe-dapu fault and Yongan-jinjiang fault were two major ore controlling faults.A series of nappe, gliding faults and folds combined with magma intrusion, providing tectonic-thermal conditions as open type, semi-open and semi-closed type and closed type for graphitization and causing the divergence of distribution and types of coal-based graphite.On the basis of the distribution of different types of coal-based graphite and influencing factors, Datian-Zhangping (Ⅰ1) and Yongan-Anxi (Ⅰ2) metallogenic belts of coal-based graphite were divided in the south-western Fujian Province, including Kekeng-Wukeng (Ⅱ1), Yongan-Datian (Ⅱ2), Changao (Ⅱ3) and Anxi (Ⅱ4) metallogenic sub-zones. © 2020, Editorial Office of Journal of China Coal Society. All right reserved.
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页码:2865 / 2871
页数:6
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共 30 条
  • [11] KWIECINSKA B, PETERSEN H I., Graphite, semigraphite, natural coke, and natural char classification-ICCP system, International Journal of Coal Geology, 57, 2, pp. 99-116, (2004)
  • [12] LANDIS C A., Graphitization of dispersed carbonaceous material in metamorphic rocks, Contributions to Mineralogy and Petrology, 30, 1, pp. 34-45, (1971)
  • [13] ZHENG Z, ZHANG J, HUANG J Y., Observations of microstructure and reflectivity of coal graphites for two locations in China, International Journal of Coal Geology, 30, 4, pp. 277-284, (1996)
  • [14] LIU Qinfu, YUAN Liang, LI Kuo, Et al., Structure characteristics of different metamorphic grade coal-based graphites, Earth Science, 43, 5, pp. 1663-1669, (2018)
  • [15] SU Xianbo, SI Qing, SONG Jinxing, Characteristics of coal Raman spectrum, Journal of China Coal Society, 41, 5, pp. 1197-1202, (2016)
  • [16] LI Xia, ZENG Fangui, WANG Wei, Et al., Raman characterization of structural evolution in the low-middle rank coals, Journal of China Coal Society, 41, 9, pp. 2298-2304, (2016)
  • [17] DONG Yeji, CAO Daiyong, WANG Lu, Et al., Indicators for partitioning graphite and anthracite in coal measures during geological exploration, Coal Geology & Exploration, 46, 1, pp. 8-12, (2018)
  • [18] RANTITSCH G, LAMMERER W, FISSLTHALER E, Et al., On the discrimination of semi-graphite and graphite by Raman spectroscopy, International Journal of Coal Geology, 159, pp. 48-56, (2016)
  • [19] BUSECK P R, BEYSSAC O., From organic matter to graphite: Graphitization, Elements, 10, pp. 421-426, (2014)
  • [20] OBERLIN A., Carbonization and graphitization, Carbon, 22, pp. 521-541, (1984)