Saturated hydrocarbon characteristics of superhigh-organic-sulfur coals in Heshan Shicun mine, Guangxi
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摘要: 以合山石村矿超高有机硫煤为研究对象,利用带能谱的扫描电镜(SEM-EDX)及气相色谱(GC)和色谱-质谱联用(GC-MS)分析技术,综合分析探讨了研究区样品中有机质来源、沉积环境及物源输入。结果表明,研究区样品镜质体反射率均值1.76%,全硫含量均值6.01%,其中有机硫含量占比达94.3%,为高成熟度的超高有机硫煤。饱和烃色谱图中未分辨的复杂混合物(UCM)鼓包明显,前峰及双峰型均有分布,前峰型主峰碳为C16、C18、C21,双峰型主峰碳为C18、C27,化合物降姥鲛烷、脱氢松香烷、咔达烯均有发现,规则甾烷C27、C28、C29均呈"V"型分布,说明沉积母质受藻类等低等水生生物与高等植物双重输入的影响。姥植比参数、C31-35藿烷呈阶梯式递减的分布特征表明在海相碳酸盐台地成煤带中存在一定的氧化条件。扫描电镜中拍摄到的铁含氧硫酸盐、细胞充填环状黄铁矿说明在沉积质晚期成岩阶段受到一定程度热液作用影响。Abstract: A superhigh-organic-sulfur (SHOS) coals were chosen to study the environmental causes of Heshan coal origin. Based on routine analysis such as scanning electron microscope (SEM-EDX) observation, gas chromatograph (GC) and gas chromatograph-mass spectrometry (GC-MS), the composition and molecular geochemical features of organic matter were analyzed to deeply reveal the organic matter sources, sedimentary environments and provenance inputs. The results indicate that the average vitrinite reflectance of the samples is 1.76%, and the average total sulfur is 6.01%, among which the organic sulfur content accounts for 94.3%, belonging to a high-maturation super high organic sulfur coal. Unresolved Complex Mixtures(UCM) bulge is obvious in the saturated hydrocarbon chromatogram, both front and bimodal peaks are found. The main carbon peaks of the front peak type are C16, C18, C21 and the bimodal is C18 and C27. Meanwhile, these compounds norpristane, dehydroabietane, cadalene have been found in samples, and regular sterane C27, C28, C29 show a "V" type distribution, which indicates that sedimentary parent material is affected by the double input of lower aquatic organisms and high plants. The distribution of hopane in C31-35 decreases stepwise, and the ratio of pristane to phytane shows that there are certain oxidation conditions in the coal-forming zone of marine carbonate platform. Fe (Si, Al)-oxysulfate and cell-filled pyrite observed by SEM indicate that the sedimentary diagenesis is affected by hydrothermal process to some extent in the diagenetic stage of late sedimentary facies.
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Key words:
- Heshan /
- superhigh-organic-sulfur /
- GC-MS /
- biomarker /
- geochemistry
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表 1 煤样品中工业分析及全硫、形态硫分析
Table 1 Proximate analysis and sulfur forms of the coals used
Sample
no.Proximate analysis /% Sulfur forms /% So/Sp So/St Ro, r/% Mad Ad Vdaf St, d Sp, d Ss, d So, d So, daf SC1 1.60 35.54 17.00 5.18 0.30 0.10 4.78 7.42 15.93 0.92 1.721 SC2 1.58 30.77 16.92 5.16 0.08 0.08 5.00 7.22 62.50 0.97 1.781 SC3 1.87 27.84 15.05 5.56 0.11 0.07 5.38 7.46 48.91 0.97 1.682 SC4 0.86 22.17 16.33 6.48 0.10 0.04 6.33 8.13 63.30 0.98 1.838 SC5 1.04 46.55 24.60 4.75 0.12 0.14 4.49 8.40 37.42 0.95 1.73 SC6 0.86 26.30 16.97 6.94 0.10 0.07 6.77 9.19 67.70 0.98 1.891 SC7 0.86 31.71 17.61 6.29 0.07 0.08 6.14 8.99 87.71 0.98 1.887 SC8 0.82 25.91 17.15 6.84 0.08 0.06 6.69 9.03 83.63 0.98 1.86 SCG1 2.06 84.01 83.68 0.43 0.12 0.12 0.18 1.13 1.50 0.42 1.624 SCG2 1.90 81.98 75.36 1.13 0.32 0.28 0.54 3.00 1.69 0.48 1.608 SCG3 1.78 85.43 91.90 0.59 0.33 0.18 0.08 0.55 0.24 0.14 1.613 SC9 3.56 40.44 23.77 6.92 0.57 1.11 5.24 8.80 9.19 0.76 1.919 Average 1.57 44.89 34.69 4.69 0.19 0.19 4.30 6.61 39.98 0.79 1.763 note: Mad=moisture; Ad=ash; Vdaf=volatile; St, d=total sulfur; Sp, d=pyritic sulfur; Ss, d=sulfate sulfur; So, d=organic sulfur 表 2 样品可溶有机抽提物含量分布
Table 2 Content of organic extracts of coal samples from Shicun
Sample no. Extr/mg Alk(% of extr) Aro(% of extr) Het(% of extr) Asph(% of extr) Alk/aro SC1 12.5 14.40 75.20 8.76 1.64 0.19 SC2 14.3 14.48 70.52 7.43 7.57 0.20 SC3 11.9 10.08 79.83 9.93 0.16 0.13 SC4 16.7 8.71 84.05 2.31 4.93 0.10 SC5 13.1 6.12 86.18 7.01 0.69 0.07 SC6 12.5 10.41 84.40 5.11 0.08 0.12 SC7 13.3 8.27 78.51 12.57 0.65 0.10 SC8 19.3 4.66 82.24 12.18 0.92 0.05 SCG1 4.3 4.65 58.84 11.90 24.61 0.08 SCG2 12.0 5.67 60.33 21.01 12.99 0.09 SCG3 2.0 5.49 67.38 22.15 4.98 0.08 SC9 16.0 19.88 75.63 3.41 1.08 0.26 note: extr=extract yield; aro=aromatic hydrocarbon fraction; alk=saturated hydrocarbon fraction; het=hetrocompounds (polar compounds); asph=asphaltenes 表 3 饱和烃参数
Table 3 Parameters of n-alkanes
Type Sample
no.Carbon Main
carbonOEP Pr/nC17 Ph/nC18 Pr/Ph ∑C22-/
∑C23+(C21+C22)/
(C28+C29)TypeⅠ SC2 C12-33 C16 0.65 0.44 0.57 1.01 4.74 1.68 SC4 C12-31 C16 0.58 0.45 0.49 0.92 6.12 2.60 SCG1 C12-33 C18 0.92 0.47 0.39 1.22 3.26 3.46 SCG3 C14-29 C21 0.81 0.48 0.42 1.61 7.34 3.97 TypeⅡ SC1 C15-34 C19 0.76 0.59 0.71 0.42 0.76 0.74 SC5 C15-36 C18, C27 1.61, 0.71 0.61 0.61 0.57 0.23 0.15 SC6 C15-35 C18, C27 1.57, 1.06 0.63 0.64 0.62 0.34 0.20 SC7 C15-35 C18, C27 1.76, 1.02 0.59 0.62 0.49 0.43 0.26 SC8 C15-35 C18, C27 0.62, 1.13 0.55 0.51 0.67 0.60 0.26 SCG2 C15-35 C18 0.72 0.53 0.56 0.82 1.33 0.69 SC9 C15-35 C18 0.76 0.64 0.79 0.72 1.36 0.84 explanation: ${\rm{OEP = }}\frac{{{{\rm{C}}_{i - 2}} + 6{{\rm{C}}_i} + {{\rm{C}}_{i + 2}}}}{{4{{\rm{C}}_{i - 1}} + 4{{\rm{C}}_{i + 1}}}}$, Ci is main carbon 表 4 研究区煤样主要生物化合物标志参数
Table 4 Main biomarker parameters of coals from research area
Samples no. Ⅰ Ⅱ Ⅲ Ⅳ Ⅴ Ⅵ Ⅶ Ⅷ Ⅸ Ⅹ Ⅺ Ⅻ SC1 0.61 1.08 0.52 0.18 0.40 0.22 0.55 34.05 26.85 39.09 0.45 0.41 SC2 0.62 0.94 0.49 0.26 0.44 0.19 0.58 40.26 27.06 32.67 0.46 0.39 SC4 1.03 1.02 0.51 0.27 0.56 0.17 0.57 29.67 35.94 34.38 0.48 0.38 SC5 0.55 1.81 0.64 0.26 0.39 0.18 0.57 33.82 26.93 39.25 0.48 0.36 SC6 0.48 1.17 0.54 0.27 0.38 0.16 0.55 33.23 28.9 37.87 0.48 0.38 SC7 0.47 1.48 0.60 0.30 0.41 0.15 0.57 35.91 29.18 34.9 0.50 0.40 SC8 0.53 1.24 0.55 0.27 0.51 0.16 0.56 38.6 27.86 33.54 0.49 0.39 SCG1 0.65 0.47 0.32 0.21 0.29 0.26 0.51 34.46 28.63 36.91 0.43 0.37 SCG2 0.66 1.17 0.54 0.32 0.43 0.19 0.54 30.19 29.23 40.57 0.49 0.35 SCG3 0.86 1.27 0.56 0.27 0.40 0.16 0.54 32.92 28.39 38.69 0.48 0.37 SC9 0.53 0.87 0.47 0.28 0.39 0.21 0.55 33.55 29.56 36.89 0.47 0.37 note: Ⅰ=C24 tetracyclic terpane/C26 tricyclic terpane; Ⅱ=Ts/Tm; Ⅲ=Ts/(Ts+Tm); Ⅳ= gammacerane/C30 hopane; Ⅴ=C23 tricyclic terpane/C30 hopane; Ⅵ=C30 moretanes/C30 hopane; Ⅶ=C31 hopane 22S/(22S+22R); Ⅷ=C27/(C27+C28+C29) sterane×100; Ⅸ=C28/(C27+C28+C29) sterane×100; Ⅹ=C29/(C27+C28+C29) sterane×100; Ⅺ=C29 sterane′s 20S/(20S+20R); Ⅻ=C29 sterane′s αββ /(ααα + αββ) -
[1] 梁汉东.超高硫煤有机相中的元素硫与铁复合物的证据[J].燃料化学学报, 2001, 29(2):108-110. http://d.old.wanfangdata.com.cn/Periodical/rlhxxb200102003LIANG Han-dong. Evidence for the complex of elemental sulfur plus iron in organic PHAS of super-high sulfur coal[J]. J Fuel Chem Technol, 2001, 29(2):108-110. http://d.old.wanfangdata.com.cn/Periodical/rlhxxb200102003 [2] LEI J J, REN D Y, TANG Y G, CHU X L, ZHAO R. Sulfur accumulating model of super high organic sulfur coal from Guiding, China[J]. Chin Sci Bull, 1994, 39(21):1817-1821. http://www.cqvip.com/QK/86894X/199421/1005017383.html [3] DAI S F, REN D Y, ZHOU Y P, CHOU C L, WANG X B, ZHAO L, ZHU X W. Mineralogy and geochemistry of a superhigh-organic-sulfur coal, Yanshan Coalfield, Yunnan, China:Evidence for a volcanic ash component and influence by submarine exhalation[J]. Chem Geol, 2008, 255(1/2):182-194. http://cn.bing.com/academic/profile?id=63f3547b39b3566c6220e0e6c5b04e3e&encoded=0&v=paper_preview&mkt=zh-cn [4] DAI S F, SEREDIN V V, WARD C R, HOWER J C, XING Y W, ZHANG W G, SONG W J, WANG P P. Enrichment of U-Se-M-Re-V in coals preserved within marine carbonate successions:Geochemical and mineralogical data from the Late Permian Guiding Coalfield, Guizhou, China[J]. Miner Deposita, 2015, 50:159-186. [5] 李彬, 韩守程, 贺鑫, 马天捧, 唐跃刚.云南砚山干河煤矿超高有机硫煤的煤岩煤质特征[J].中国煤炭地质, 2016, 28(1):6-12. http://d.old.wanfangdata.com.cn/Periodical/zgmtdz201601002LI Bin, HAN Shou-cheng, HE Xin, MA Tian-peng, TANG Yue-gang. Coal petrology and coal quality characteristics of superhigh organic coal in Ganhe coalmine, Yanshan, Yunnan[J]. Coal Geol China, 2016, 28(1):6-12. http://d.old.wanfangdata.com.cn/Periodical/zgmtdz201601002 [6] 雷加锦, 濮英英, 任德贻.贵定超高有机硫煤中的细菌体及其意义[J].岩石学报, 1995, 11(4):456-461. http://www.cnki.com.cn/Article/CJFDTotal-YSXB199504010.htmLEI Jia-jin, PU Ying-ying, REN De-yi. Bacterium-like bodies and its significance in high organosulfur coal from Guiding[J]. Acta Pet Sin, 1995, 11(4):456-461. http://www.cnki.com.cn/Article/CJFDTotal-YSXB199504010.htm [7] 张卫国, 杨建业, 石媛.广西合山超高有机硫煤中稀土元素特征[J].稀土, 2019, 40(2):49-56. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xitu201902006ZHANG Wei-guo, YANG Jian-ye, SHI Yuan. Characteristics of rare earth elements in super high organic sulfur coal in guangxi[J]. Chin Rare Earth, 2019, 40(2):49-56. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xitu201902006 [8] 黄乃和, 温显端.广西合山碳酸盐岩型煤组的沉积环境[J].煤田地质与勘探, 1980, 2:1-7+2-101. http://www.cnki.com.cn/Article/CJFDTotal-MDKT198002000.htmHUANNG Nai-he, WEN Xian-duan. Carbonate briquette group sedimentary environment of Heshan, Guangxi[J]. Coal Geol Explor, 1980, 2:1-7+2-101. http://www.cnki.com.cn/Article/CJFDTotal-MDKT198002000.htm [9] SHAO L Y, TIM J, ROD G, DAI S F, LI S S, JIANG Y F, ZHANG P F. Petrology and geochemistry of the high-sulphur coals from the Upper Permian carbonate coal measures in the Heshan coalfield, southern China[J]. Int J Coal Geol, 2003, 55(1):1-26. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=82389b6b1fcc872cecf525de7ceeceef [10] ZENG R S, ZHANG X G, KOUKOUZAS N, XU W D. Characterization of trace elements in sulphur-rich Late Permian coals in the Heshan coal field, Guangxi, South China[J]. Int J Coal Geol, 2005, 61(1/2):87-95. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ea05622cd95391c72f5a35c1ab3327ac [11] DAI S F, ZHANG W G, SEREDIN V V, WARD C R, HOWER J C, SONG W J, WANG X B, LI X, KANG H, ZHENG L C, WANG P P, ZHOU D. Factors controlling geochemical and mineralogical compositions of coals preserved within marine carbonate successions:A case study from the Heshan Coalfield, Southen China[J]. Int J Coal Geol, 2013, 109:77-100. https://www.sciencedirect.com/science/article/abs/pii/S0166516213000438 [12] ZHAO Q J, NIU Y J, XIE Z Z, ZHANG K M, ZHOU J M, ARBUZOV S I. Geochemical characteristics of elements in coal seam 41 and 42 of Heshan Coalfield, South China[J]. Energy Explor Exploit, 2020, 38(1):137-157. https://www.researchgate.net/publication/337282110_Geochemical_characteristics_of_elements_in_coal_seams_4_1_and_4_2_of_Heshan_Coalfield_South_China [13] KONTENSKI J, KOSTOVA I. Occurrence and morphology of pyrite in Bulgarian coals[J]. Int J Coal Geol, 1996, 29(4):273-290. http://cn.bing.com/academic/profile?id=272f8b486dad2674629c8c5b3e19b40e&encoded=0&v=paper_preview&mkt=zh-cn [14] 葛运培, 谢光前, 曾百亨, CHARLES A W.煤中黄铁矿及其毗邻的有机硫[J].燃料化学学报, 1992, 20(1):92-97. http://www.cnki.com.cn/Article/CJFDTotal-RLHX199201013.htmGE Yun-pei, XIE Guang-qian, ZENG Bai-heng, CHARLES A W. The pyrite in the coal and organic sulfur in its vicinity[J]. J Fuel Chem Technol, 1992, 20(1):92-97. http://www.cnki.com.cn/Article/CJFDTotal-RLHX199201013.htm [15] 袁利.黔西南高硫煤的地质成因-黄铁矿与硫同位素分析[D].徐州: 中国矿业大学, 2014.YUAN Li. Geological genesis of the high sulfur coal from southwestern Guizhou-Analysis of pyrite and sulfur isotope[D]. Xuzhou: China University of Mining and Technology, 2014. [16] 倪建宇, 洪业汤.贵州晚二叠世煤中硫同位素的组成特征[J].地质地球化学, 1999, 27(2):63-69. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900079509NI Jian-yu, HONG Ye-tang. Sulfur isotopic composition of late Permian coal from Guizhou province[J]. Geol Geochem, 1999, 27(2):63-69. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900079509 [17] 肖贤明, 毛鹤龄.从各向异性壳质组的发现论壳质组在煤化过程中的光性演变[J].沉积学报, 1991, 9(1):87-96. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000030048XIAO Xian-ming, MAO He-ling. Optical evolution of exinite euring coalification based on the discovery of the an isotropical exinite[J]. Acta Sedimentol Sin, 1991, 9(1):87-96. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000030048 [18] 刘朝林, 姚志温, 吴德云.安徽省主要煤种的有机地球化学特征与煤成气的关系[J].沉积学报, 1983, 1(2):17-30. http://www.cnki.com.cn/Article/CJFDTotal-CJXB198302001.htmLIU Chao-lin, YAO Zhi-wen, WU De-yun. Relationship between organic geochemical characteristics and coal gasification of main coal species in Anhui province[J]. Acta Sedimentol Sin, 1983, 1(2):17-30. http://www.cnki.com.cn/Article/CJFDTotal-CJXB198302001.htm [19] 贾继红, 白益军, 王晓锋, 张平中, 桑文翠, 张德忠, 张虹, 王永莉, 孟仟祥.若尔盖高原湖沼沉积剖面饱和烃组分特征及地球化学意义[J].沉积学报, 2012, 30(4):755-760. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201204018JIA Ji-hong, BAI Yi-jun, WANG Xiao-feng, ZHANG Ping-zhong, SANG Wen-cui, ZHANG De-zhong, ZHANG Hong, WANG Yong-li, MENG Qian-xiang. Geochemical significance of the Saturated Hydrocarbons of Limnological Sediments from Ruoergai Plateau[J]. Acta Sediment Sin, 2012, 30(4):755-760. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201204018 [20] ZHANG M, HUANG G H, LI H B, HU G Y, ZHANG S C. Molecular geochemical characteristics of gas source rocks from the upper triassic xujiahe formation indicate transgression events in the sichuan basin[J]. Sci China Ser D:Earth Sci, 2012, 55(8):1260-1268. http://cn.bing.com/academic/profile?id=d77b5ebb31d5a3ee718fce47dd9dd5a1&encoded=0&v=paper_preview&mkt=zh-cn [21] 李薇薇.辰溪特高有机硫煤的地球化学特征与硫的成因[D].北京: 中国矿业大学, 2013.LI Wei-wei. Geochemistry of Super-high-organic-sulfur Coals from Chenxi, Hunan and Gelogical Origin of the Sulfur[D]. Beijing: China University of Mining and Technology, 2013. [22] 何瑜, 张敏, 陈小慧, 龚建明, 李永红, 王伟超, 雷天柱.青海木里冻土区煤系烃源岩饱和烃地球化学特征[J].科学技术与工程, 2015, 32(15):121-128. http://d.old.wanfangdata.com.cn/Periodical/kxjsygc201532022HE Yu, ZHANG Min, CHEN Xiao-hui, GONG Jian-ming, LI Yong-hong, WANG Wei-chao, LEI Tian-zhu. Geochemical characteristics of saturated hydrocarbon in coal-measure source rocks from muli permafrost, Qinghai[J]. Sci Technol Eng, 2015, 32(15):121-128. http://d.old.wanfangdata.com.cn/Periodical/kxjsygc201532022 [23] XIE S C, WANG Z Y, WANG H M, CHEN F H, AN C B. The occurrence of a grassy vegetation over the chinese loess plateau since the last interglacier:The molecular fossil record[J]. Sci China Ser D:Earth Sci, 2002, 45(1):53-62. http://cn.bing.com/academic/profile?id=accd98198c52d94454208c3ceb4dbe9a&encoded=0&v=paper_preview&mkt=zh-cn [24] 董家国.合山煤田首次发现植物化石[J].煤田地质与勘探, 1984, (1):2. http://www.cnki.com.cn/Article/CJFDTotal-MDKT198401000.htmDONG Jia-guo. Plant fossils were first discovered in Heshan Coalfield[J]. Coal Geol Explor, 1984, (1):2. http://www.cnki.com.cn/Article/CJFDTotal-MDKT198401000.htm [25] 卓越.桂中晚二迭世合山组沉积特征和成煤环境[J].煤田地质与勘探, 1980, (3):1-7. http://www.cnki.com.cn/Article/CJFDTotal-MDKT198003000.htmZHUO Yue. Sedimentary characteristics and coal-forming environment of the Heshan formation in the Middle Perm, Guizhou[J]. Coal Geol Explor, 1980, (3):1-7. http://www.cnki.com.cn/Article/CJFDTotal-MDKT198003000.htm [26] 王汇彤, 张水昌, 翁娜, 魏小芳, 朱光有, 于菡, 毕丽娜, 马文玲.稠油中饱和烃复杂混合物成分解析及其意义[J].中国科学:化学, 2012, 42(10):1469-1478. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cb201210009WANG Hui-tong, ZHANG Shui-chang, WENG Na, WEI Xiao-fang, ZHU Guang-you, YU Han, BI Li-na, MA Wen-ling. Insight of unresolved complex mixtures of saturated hydrocarbons in heavy oil via GCxGC-TOF MS analyses[J]. Sci China-Chem, 2012, 42(10):1469-1478. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cb201210009 [27] 桑树勋, 刘焕杰, 施健.海南岛红树林泥炭中硫及其成因研究[J].煤田地质与勘探, 1993, 21(1):12-17. http://www.cnki.com.cn/Article/CJFD1993-MDKT199301004.htmSANG Shu-xun, LIU Huan-jie, SHI Jian. Study of sulphur and its genesis in mangrove peats of Hainan island[J]. Coal Geol Explor, 1993, 21(1):12-17. http://www.cnki.com.cn/Article/CJFD1993-MDKT199301004.htm [28] PETERS K E, WALTERS C C, MOLDWAN J M. The Biomarker Guider(2nd Edition)[M]. New York: Cambridge University Press, 2005. [29] 陈菊林.热力作用对烃源岩中重排藿烷类化合物组成影响及形成机理研究[D].荆州: 长江大学, 2017.CHEN Ju-lin. Thermal Effect on Rearranged Hopanes Composition in source rocks and study on its Formation mechanism[D]. Jingzhou: Yangtze University, 2017. [30] PETERS K E, MOLDOWAN J M. The Biomarker Guide: Interpreting Molecular Fossils in Petroleum and Ancient Sediments[M]. New Jersey: Prentice Hall, 1993. [31] 张立平, 黄第藩, 廖志勤.伽马蜡烷-水体分层的地球化学指标[J].沉积学报, 1999, 17(1):136-140. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb199901022ZHANG Li-ping, HUANG Di-fan, LIAO Zhi-qin. Gammacerane-geochemical indicator of water column stratification[J]. Acta Sediment Sin, 1999, 17(1):136-140. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb199901022 [32] VOLKMAN J K. Biological marker compounds as indicators of the depositional environments of petroleum source rocks[J]. Geol Soc London Spe Pub, 1988, 40(1):103-122. http://cn.bing.com/academic/profile?id=09dee6bbece7977af38575ad84ef332a&encoded=0&v=paper_preview&mkt=zh-cn [33] PETERS K E, MOLDWAN J M, SUNDARARAMAN P. Effects of hydrous pyrolysis on biomarker thermal maturity parameters:Monterey phosphatic and siliceous members[J]. Org Geochem, 1990, 15(3):249-265. http://cn.bing.com/academic/profile?id=3052ae56c124dde7581b8094404061f2&encoded=0&v=paper_preview&mkt=zh-cn