stressors
发表于 2025-3-23 13:42:05
http://reply.papertrans.cn/67/6620/661966/661966_11.png
刺激
发表于 2025-3-23 15:42:57
http://reply.papertrans.cn/67/6620/661966/661966_12.png
Host142
发表于 2025-3-23 21:49:36
http://reply.papertrans.cn/67/6620/661966/661966_13.png
Homocystinuria
发表于 2025-3-23 23:35:04
http://reply.papertrans.cn/67/6620/661966/661966_14.png
Cacophonous
发表于 2025-3-24 04:45:29
http://reply.papertrans.cn/67/6620/661966/661966_15.png
Ambiguous
发表于 2025-3-24 06:44:45
http://reply.papertrans.cn/67/6620/661966/661966_16.png
NIB
发表于 2025-3-24 12:49:52
High Temperature Pyrolysis of Oil Shales,em becomes even more complex as shales contain only a relatively small percentage of organic matter and the rest is inorganic minerals. Moreover, usually shale deposits have considerable nitrogen and sulfur containing compounds, and these have to be eliminated before the products can be used.
Discrete
发表于 2025-3-24 16:03:29
Formation of Young Kerogen: Protein-Based Melanoidin Hypothesis and Heating Experiments Under Mild .g. Blumer, 1973; Hunt, 1996; Tissot and Weite, 1984). Kerogen classifications and its thermal alterations leading to liquid and gaseous products have been extensively investigated by a number of authors (e.g. Tissot and Weite, 1984; Hunt, 1996). These investigations enriched greatly the knowledge of chemistry and geochemistry of kerogen.
身心疲惫
发表于 2025-3-24 20:39:37
http://reply.papertrans.cn/67/6620/661966/661966_19.png
共同给与
发表于 2025-3-25 00:47:39
Book 2003-Pyrolysis of oil-shales; .-Formation of coal and its gasification and liquification; .-Thermal liquification of biomass; .-Geothermal energy; .-Thermal generation of fullerenes; .-Thermal formation of diamonds; .-Thermal analysis of organo-clay complexes; .-Geochemical conditions for life emergence..