| 黔北地区下志留统龙马溪组烃源岩生物标志物 |
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| 引用本文： | 林家善,谢渊,刘建清,赵瞻,景小燕.黔北地区下志留统龙马溪组烃源岩生物标志物[J].沉积与特提斯地质,2010,30(4):109-112. |
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| 作者姓名： | 林家善 谢渊 刘建清 赵瞻 景小燕 |
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| 作者单位： | [1]成都地质矿产研究所,四川成都610081 [2]中国石化西南油气分公司勘探开发研究院,四川成都610081 |
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| 摘 要： | 应用气相色谱和色谱-质谱分析技术,对黔北地区下志留统龙马溪组烃源岩的甾烷和萜烷进行测试分析。结果表明,正构烷烃为后单峰型,主峰碳为C22～C30,Pr/Ph值为0.48～0.64,Pr/nC17为1.35～4.22,Ph/nC18为0.92～0.97。甾烷中,具孕烷系列的异常高值,C27、C28和C29呈规则甾烷"V"字型分布(C27C28C29),具明显的C27优势,甾烷/藿烷比值为0.57～0.71。萜烷类中具三环萜烷高值,低升藿烷,高伽马蜡烷指数特征。成熟度方面,OPE1,Ts/(Ts+Tm)分布在0.42～0.48之间,C3122S/(S+R)值为0.6～0.66,C29ββ/(ββ+αα)在0.56～0.58之间,反映出龙马溪期具明显的水体分层和高还原环境。有机质主要来源于浮游水生生物和藻类,并经历了一定的生物降解过程。烃源岩的热演化已进入高成熟-过成熟阶段。
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| 关 键 词： | 黔北地区 龙马溪组 烃源岩 生物标志物 |
The biomarkers in the source rocks from the Lower Silurian Longmaxi Formation in northern Guizhou |
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| LIN Jia-shan,XIE Yuan,LIU Jian-qing,ZHAO Zhan,JING Xiao-yan.The biomarkers in the source rocks from the Lower Silurian Longmaxi Formation in northern Guizhou[J].Sedimentary Geology and Tethyan Geology,2010,30(4):109-112. |
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| Authors: | LIN Jia-shan XIE Yuan LIU Jian-qing ZHAO Zhan JING Xiao-yan |
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| Institution: | 1.Chengdu Institute of Geology and Mineral Resources,Chengdu 610081,Sichuan,China;2.Southwest Oil ＆ Gas Field Company,PetroChina,Chengdu 610081,Sichuan,China) |
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| Abstract: | The steranes and terpanes in the source rocks from the Lower Silurian Longmaxi Formation in northern Guizhou are determined with the aid of gas chromatography and chromatography-mass spectrographic analysis.The analytical results suggest that the n-alkanes in the source rocks display a back single-peak pattern,with the main peak carbon values ranging from C22 to C30.The Pr/Ph ratios vary from 0.48 to 0.64;Pr/nC17 ratios vary from 1.35 to 4.22,and Ph/nC18 ratios vary from 0.92 to 0.97.The pregnane and homopregnane are very rich in steranes.C27,C28 and C29 display a regular V-type distribution pattern（C27 C28 C29）,with a C27 dominance.The sterane/aromadendrane ratios range between 0.57 and 0.71.The terpanes are characterized by high tricycloterpane values,low aromadendrane values and high gammacerane indexes.All the values for the maturity such as OPE1,Ts/（Ts ＋ Tm） ratios ranging between 0.42 and 0.48,C3122S/（S ＋ R） ratios ranging between 0.6 and 0.66,and C29 ββ/（ββ ＋αα） ratios ranging between 0.56 and 0.58 indicate the stratified water bodies and highly reduced conditions during the Longmaxian.The organic matter dominantly came from planktons and algae,and has been subjected to a certain degree of biodegradation.The thermal evolution of the source rocks has reached up to the stages of high maturation and overmaturation. |
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| Keywords: | northern Guizhou Longmaxi Formation source rock biomarker |
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