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English: Original legend: Macerals in the Upper No. 3 coals. (A) Sporinite, corpogelinite, inertodetrinite, and colledetrinite (LBS3U-4); (B) Sporinite under fluorescent light (LBS3U-4); (C) Cutinite, sporinite, and colledetrinite (LBS3U-13); (D) Cutinite and sporinte under fluorescent light (LBS3U-13); A, C, are under oil reflectance white light.
Date Manuscript Received: 18 April 2016 / Revised: 22 May 2016 / Accepted: 16 June 2016 / Published: 23 June 2016
Source Figure 5a from the following scientific paper: Mineralogical and Geochemical Characteristics of the Early Permian Upper No. 3 Coal from Southwestern Shandong, China. Minerals 2016, 6(3), 58; https://doi.org/10.3390/min6030058
Author Xibo Wang1, Lili Zhang1, Yaofa Jiang2, Jianpeng Wei1, and Zijuan Chen1, from the following institutions: 1) State Key laboratory of Coal Resources and Safety Mining, China University of Mining and Technology, Beijing 100083, China; 2) Jiangsu Institute of Architectural Technology, Xuzhou 221116, China
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current17:01, 31 May 2018Thumbnail for version as of 17:01, 31 May 20182,711 × 2,069 (5.73 MB)Dietzel65{{Information |description ={{en|1=Original legend: Macerals in the Upper No. 3 coals. (A) Sporinite, corpogelinite, inertodetrinite, and colledetrinite (LBS3U-4); (B) Sporinite under fluorescent light (LBS3U-4); (C) Cutinite, sporinite, and colledetrinite (LBS3U-13); (D) Cutinite and sporinte under fluorescent light (LBS3U-13); (E) Resinite, inertodetrinite, sporinite, semifusinite and colledetrinte (LBS3U-6); (F) Resinite and sporinite under fluorescent light (LBS3U-6); (G) Secretinite, s...

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