龙马溪组烃源岩对川中地区长兴组天然气成藏的贡献:来自华蓥山沥青抽提物生物标志化合物的证据OA
Contribution of Longmaxi Formation source rocks to gas accumulation in Changxing Formation,central Sichuan Basin:Evidence from biomarkers of bitumen extracts from Huayingshan area
为了厘清志留系下统龙马溪组烃源岩对四川盆地川中地区二叠系上统长兴组气藏有无贡献,利用龙马溪组、二叠系中统茅口组、二叠系上统龙潭组烃源岩以及华蓥山区域涧水沟剖面长兴组固体沥青的气相色谱—质谱测试结果确定长兴组固体沥青的来源,进而验证龙马溪组烃源岩对长兴组气藏的贡献.研究结果表明:①龙马溪组烃源岩沉积水体盐度最低,其有机质有较高的红藻贡献,茅口组烃源岩沉积水体盐度最高,绿藻是其重要的生烃母质,而龙潭组烃源岩沉积水体盐度中等,有机质主要来源于红藻、绿藻以及高等植物等;②华蓥山区域涧水沟剖面长兴组固体沥青为热化学蚀变成因,主要来源于龙马溪组烃源岩;③深大断裂是深部油气垂向运移的有利通道,可以将龙马溪组烃源岩生成的油气输导至长兴组成藏.结论认为,深大断裂可以将龙马溪组烃源岩生成的油气输导至长兴组成藏;绵阳—广安浅水陆棚东部边缘带发育断至长兴组的深大断裂且该区龙马溪组烃源岩品质较好,有利于天然气成藏,因而长兴组天然气勘探潜力值得重视.
In order to clarify whether the Lower Silurian Longmaxi Formation source rocks have contributed to the Upper Permian Changxing Formation gas reservoirs in the central Sichuan Basin,gas chromatography-mass spectrometry(GC-MS)tests were conducted on source rocks from the Longmaxi Formation,Middle Permian Maokou Formation,and Upper Permian Longtan Formation,as well as solid bitumen from the Changxing Formation in the Jianshuigou section of the Huayingshan area.The source of solid bitumen in the Changxing Formation was identified to verify the contribution of Longmaxi Formation source rocks to Changxing Formation gas reservoirs.The following results are obtained.(i)The Longmaxi Formation source rocks are deposited in the lowest salinity water body,showing relatively high organic matter contribution from red algae;the Maokou Formation source rocks are deposited in the highest salinity water body,with green algae being an important hydrocarbon-generating parent material;whereas the Longtan Formation source rocks are deposited in water body with moderate salinity,with organic matter mainly supplied from red algae,green algae,and higher plants.(ii)The Changxing Formation solid bitumen in the Jianshuigou section of the Huayingshan area is of thermochemical alteration origin,primarily derived from the Longmaxi Formation source rocks.(iii)Deep-seated faults serve as favorable vertical migration pathways for deep hydrocarbons,enabling the transport of hydrocarbons generated by the Longmaxi Formation source rocks to the Changxing Formation for accumulation.It is concluded that the deep-seated faults can transport the hydrocarbons generated by the Longmaxi Formation source rocks to the Changxing Formation for accumulation.Eastern margin of the Mianyang-Guang'an shallow-water shelf,where deep-seated faults extending into the Changxing Formation are developed and the Longmaxi Formation source rocks are of high quality,is conducive to gas accumulation.Therefore,the exploration potential of Changxing Formation gas reservoirs deserves attention.
文华国;李长志;张玺华;孙豪飞;邓思思
成都理工大学沉积地质研究院 四川 成都 610059||油气藏地质及开发工程全国重点实验室(成都理工大学) 四川 成都 610059成都理工大学地球与行星科学学院 四川 成都 610059中国石油西南油气田公司勘探开发研究院 四川 成都 610041中国石油西南油气田公司勘探开发研究院 四川 成都 610041中国石油西南油气田公司勘探开发研究院 四川 成都 610041
能源科技
生物标志化合物四川盆地二叠系上统长兴组气藏固体沥青志留系下统龙马溪组烃源岩
BiomarkerSichuan BasinUpper Permian Changxing Formation gas reservoirSolid bitumenLower Silurian Longmaxi Formation source rock
《天然气勘探与开发》 2026 (2)
75-87,13
四川省自然科学基金项目"不同成因固体沥青微观结构差异性研究"(编号:2024NSFSC0813).
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