济阳坳陷晚古生代—中生代构造演化特点
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摘要
利用奥陶系和石炭系灰岩地层中的垂直缝合线构造,对济阳坳陷古生代古构造应力场进行的判别结果表明,自奥陶纪开始华北克拉通盆地就受到NNE—SSW向的水平挤压而整体抬升,在遭受长达140Ma的剥蚀作用后,即至晚古生代古构造应力场仍未发生改变。对地震剖面、断层活动特点以及火山活动的研究表明,晚三叠世济阳坳陷区挤压作用达到最强;早侏罗世—中侏罗世是构造转换过渡期;晚侏罗世开始以近南北向的伸展作用为特征,这是华北东部地区地幔柱上涌的结果。利用岩石薄片数据对晚古生代和中生代物源区性质和构造背景进行了判别。结果表明,石炭-二叠纪物源区性质为再旋回造山带和破裂岩浆弧;中生代物源区性质为再旋回造山带和岩浆弧,古老的基底陆块尚未遭受明显的剥蚀,说明济阳坳陷为活动大陆边缘陆相盆地。
The Paleozoic tectonic stress field was reconstructed with the vertical stylolite structure found in the Ordovician and Carboniferous limestone.The identification of Paleozoic tectonic stress field showed that North China craton suffered the horizontal compression in the NNE-SSW direction and uplifted at the beginning of the Ordovician.Then it had suffered erosion for 140 Ma until the Late Paleozoic era.The analyses on the seismic section,the action rate of faults and the volcanic activity indicated that the squeezing action was the strongest in Late Triassic of Jiyang Depression,and the Early-Middle Jurassic was the tectonic transition period.In the Late Jurassic,Jiyang Depression was featured by the extension in the south-north direction,which resulted from the upwelling of mantle plume in the eastern region of North China.The provenance nature and tectonic setting from discrimination of the rock slice data in the Late Paleozoic and Mesozoic showed that the Permian-Carboniferous provenance was natured to the recycled orogen and dissected arc.The Mesozoic provenance was natured to the recycled orogen and magma arc.The ancient basement blocks in the Mesozoic suffered little erosion,which showed that Jiyang Depression was the terrestrial basin of active continental margin.
The Paleozoic tectonic stress field was reconstructed with the vertical stylolite structure found in the Ordovician and Carboniferous limestone.The identification of Paleozoic tectonic stress field showed that North China craton suffered the horizontal compression in the NNE-SSW direction and uplifted at the beginning of the Ordovician.Then it had suffered erosion for 140 Ma until the Late Paleozoic era.The analyses on the seismic section,the action rate of faults and the volcanic activity indicated that the squeezing action was the strongest in Late Triassic of Jiyang Depression,and the Early-Middle Jurassic was the tectonic transition period.In the Late Jurassic,Jiyang Depression was featured by the extension in the south-north direction,which resulted from the upwelling of mantle plume in the eastern region of North China.The provenance nature and tectonic setting from discrimination of the rock slice data in the Late Paleozoic and Mesozoic showed that the Permian-Carboniferous provenance was natured to the recycled orogen and dissected arc.The Mesozoic provenance was natured to the recycled orogen and magma arc.The ancient basement blocks in the Mesozoic suffered little erosion,which showed that Jiyang Depression was the terrestrial basin of active continental margin.
引文
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[4]张克鑫,漆家福,马宝军,等.济阳坳陷桩海地区构造演化特征研究[J].西安石油大学学报:自然科学版,2005,20(3):40-43.Zhang Kexin,Qi Jiafu,Ma Baojun,et al.Study on the tectonic e-volution of Zhuanghai area in Jiyang Depression[J].Journal ofXi’an Shiyou University:Natural Science Edition,2005,20(3):40-43.
[5]王世虎,夏斌,陈根文,等.济阳坳陷构造特征及形成机制讨论[J].大地构造与成矿学,2004,28(4):428-434.Wang Shihu,Xia Bin,Chen Genwen,et al.Characteristics of Jiy-ang Depression and mechanism of basin formation[J].Geotecton-ica et Metallogenia,2004,28(4):428-434.
[6]王颖,赵锡奎,高博禹.济阳坳陷构造演化特征[J].成都理工学院学报,2002,29(2):181-187.Wang Ying,Zhao Xikui,Gao Boyu.Characters of tectonic evolu-tion of the Jiyang Depression[J].Journal of Chengdu Universityof Technology,2002,29(2):181-187.
[7]宗国洪,肖焕钦,李常宝,等.济阳坳陷构造演化及其大地构造意义[J].高校地质学报,1999,5(3):275-282.Zong Guohong,Xiao Huanqin,Li Changbao,et al.Evolution ofJiyang Depression and its tectonic implications[J].GeologicalJournal of China Universities,1999,5(3):275-282.
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[9]杨超,陈清华.济阳坳陷构造演化及其构造层的划分[J].油气地质与采收率,2005,12(2):9-12.Yang Chao,Chen Qinghua.Tectonic evolution and tectono-strati-graphic classification of Jiyang Depression[J].Petroleum Geolo-gy and Recovery Efficiency,2005,12(2):9-12.
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[13]Railsback L B,Hood E C.Vertical sutured contacts caused by in-tergranular pressure dissolution during tectonic compression inJurassic limestones,High Atlas Mountains,Morocco[J].Geol.Soc.Amer.Abstracts w.Programs,1993,25:A-162.
[14]Railsback L B.Tectonic stylolites perpendicular to modern stressin the“undeformed”Nashville Dome:Evidence for Jurassic-to-recent intraplate tectonic compression[J].Geol.Soc.Amer.Ab-stracts w.Programs,1995,27:A-217.
[15]Railsback L B,Andrews L M.Tectonic stylolites in the“unde-formed”Cumberland Plateau of Southern Tennessee[J].Journalof Structural Geology,1995,17(6):911-915.
[16]李国蓉.碳酸盐岩中缝合线的形成机制及其储集意义讨论[J].矿物岩石,1997,17(2):49-54.Li Guorong.Discussion on the genetic mechanism of stylolites incarbonate rocks and their significance for storage[J].Journal ofMineralogy and Petrology,1997,17(2):49-54.
[17]覃建雄,杨作升.鄂尔多斯碳酸盐岩去白云石化及其与储集性的关系[J].石油与天然气地质,1997,18(4):319-325.Qin Jianxiong,Yang Zuosheng.Dedolomitization of carbonaterocks in Ordos and its relation to reservoir property[J].Oil&Gas Geology,1997,18(4):319-325.
[18]高岗.缝合线对碳酸盐岩油气生排运聚的作用[J].西安石油学院学报:自然科学版,2000,15(4):32-34.Gao Gang.Effects of stylolites on the generation,discharge,mi-gration and accumulation of hydrocarbon in carbonate rock[J].Journal of Xi’an Petroleum Institute:Natural Science Edition,2000,15(4):32-34.
[19]曹忠祥,刘华,王玉林.济阳坳陷石炭二叠系沉积与层序地层分析[J].山东科技大学学报:自然科学版,2002,21(2):68-71.Cao Zhongxiang,Liu Hua,Wang Yulin.Sedimentation and strati-graphic sequence analysis of Permo-Carboniferous System in Jiy-ang Depression[J].Journal of Shandong University of Scienceand Technology:Natural Science,2002,21(2):68-71.
[20]Dickinson W R,Beard L S,Brakenridge G R,et al.Provenancesof North American Phanerozoic sandstones in relation to tectonicsetting[J].Geol.Soc.Am.Bull.1983,94(2):222-235.
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[22]谯汉生,纪友亮,姜在兴.中国东部大陆裂谷与油气[M].北京:石油工业出版社,1999:21-70.Qiao Hansheng,Ji Youliang,Jiang Zaixing.Rift valley with oiland gas in Eastern Mainland China[M].Beijing:Petroleum In-dustry Press,1999:21-70.
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