鲁西隆起与济阳坳陷箕状断陷形成时代研究
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摘要
箕状断陷是鲁西隆起和济阳坳陷最主要的构造样式。利用野外剖面观察、室内地质剖面分析、地震剖面分析以及裂变径迹年代学等方法对鲁西隆起和济阳坳陷箕状断陷的形成时代进行了探讨。结果表明,鲁西隆起的箕状断陷发育在本区沉积的最新地层官庄组沉积之后(即始新世以来),与距今42～38 Ma发生的蒙山抬升事件有关。济阳坳陷的箕状断陷形成时代为沙三段至东营组沉积时期,大约为距今42～24.6Ma。由此可见,鲁西隆起和济阳坳陷箕状断陷的形成时代一致,均为距今42～24.6Ma。
The dustpan fault depression is the most important tectonic style in Luxi Uplift and Jiyang Depression.The field profile observation,indoor geological profile analysis,seismic profile analysis and the fission-track dating were used to study the formation age of dustpan fault depression.The results showed that the dustpan fault depression of Luxi Uplift was developed after deposition of Guanzhuang Formation(since the Eocene) and related with the Mengshan Uplift incident generated in the period from 42 Ma to 38 Ma before present.The dustpan fault depression in Jiyang Depression was formed after deposition of Shahejie Formation and before deposition of Dongying Formation in the period of about 42 Ma to 24.6Ma before present.Therefore,the dustpan fault depression in Luxi Uplift and Jiyang Depression were formed in the period of 42 Ma to 24.6 Ma before present.
The dustpan fault depression is the most important tectonic style in Luxi Uplift and Jiyang Depression.The field profile observation,indoor geological profile analysis,seismic profile analysis and the fission-track dating were used to study the formation age of dustpan fault depression.The results showed that the dustpan fault depression of Luxi Uplift was developed after deposition of Guanzhuang Formation(since the Eocene) and related with the Mengshan Uplift incident generated in the period from 42 Ma to 38 Ma before present.The dustpan fault depression in Jiyang Depression was formed after deposition of Shahejie Formation and before deposition of Dongying Formation in the period of about 42 Ma to 24.6Ma before present.Therefore,the dustpan fault depression in Luxi Uplift and Jiyang Depression were formed in the period of 42 Ma to 24.6 Ma before present.
引文
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[16]宗国洪，石红霞，郭元玲，等．济阳坳陷地震勘探效果分析[J]．新疆石油地质，2002，23(6)：511-512．Zong Guohong,Shi Hongxia,Guo Yuanling,et al.Analysis of seismic prospecting effectiveness in Jiyang Depression[J].Xin- jiang Petroleum Geology,2002,23(6):511-512.
[2]潘元林，孔凡仙，杨申镳．中国隐蔽油气藏[M]．北京：地质出版社，1998：76-167．Pan Yuanlin,Kong Fanxian,Yang Shenbiao.Subtle reservoir in China[M].Beijing:Geological Publishing House,1998:76-167.
[3]彭传圣．箕状断陷盆地缓坡带层序格架特征与演化——以济阳坳陷为例[J]．东华理工学院学报：自然科学版，2005，28(3)：239- 243．Peng Chuansheng.Sequence framework feature and evolution of the ramp belt of half-graben-basin——example of Jiyang Depres- sion[J].Journal of East China Institute of Technology:Natural Science Edition,2005,28(3):239-243.
[4]张宇．济阳坳陷缓坡带构造特征及分类[J]．断块油气田，2005，12(3)：22-24．Zhang Yu.Structural features and classification of the gentle slope zone in Jiyang Depression[J].Fault-Block Oil & Gas Field,2005,12(3):22-24.
[5]秦永霞，姜素华，王永诗．斜坡带油气成藏特征与勘探方法——以济阳坳陷为例[J]．海洋石油，2003，23(2)：14-20．Qin Yongxia,Jiang Suhua,Wang Yongshi.Pool-forming features and exploration methods for oil and gas in slope zone[J].Off- shore Oil,2003,23(2):14-20.
[6]张一伟．山东西部箕状凹陷形成的探讨——初论地壳波状运动[J]．石油学报，1983，4(4)：19-25．Zhang Yiwei.On the formation of dustpan-shaped depressions in the western part of Shandong——a preliminary discussion on wave-like crustal movement[J].Acta Petrolei Sinica,1983,4 (4):19-25.
[7]李德生．渤海湾含油气盆地的构造格局[J]．石油勘探与开发，1979，6(2)：51-62．Li Desheng.The tectonic framework of the petroliferous basins in the Bohai Bay[J].Petroleum Exploration and Development, 1979,6(2):51-62.
[8]丁林．裂变径迹定年方法的进展及应用[J]．第四纪研究，1997，8 (3)：272-280．Ding Lin.Advance of fission-track analysis method and its appli- cation[J].Quaternary Sciences,1997,8(3):272-280.
[9]Gleadow A J W,Duddy I R,Green P F,et al.Confined fission track lengths in apatite:A diagnostic tool for thermal history a nalysis[J].Contribution to Mineralogy and Petrology,1986,94 (4):405-415.
[10]Corrigan Jeff.Inversion of apatite fission track data for thermal history information[J].Journal of Geophysical Research,1991, 96(B6):10347-10360.
[11]Gallagher Kerry.Evolving temperature histories from apatite fis- sion-track data[J].Earth and Planetary Science Letters,1995, 136(3/4):421-435.
[12]李理，钟大赉．泰山新生代抬升的裂变径迹证据[J]．岩石学报，2006，22(2)：457-464．Li Li,Zhong Dalai.Fission track evidence of Cenozoic uplifting e- vents of the Taishan Mountain,China[J].Acta Petrologica Sini- ca,2006,22(2):457-464.
[13]Belton D X.TASC:Theory and application of the track age spec- tra calculation[M].Melbourne:The University of Melbourne Press,2005:1-32.
[14]王国芝．济阳坳陷陈家庄—白庙地区构造成因及构造演化研究[D]．东营：中国石化胜利油田地质科学研究院，2006．Wang Guozhi.The structural genesis and structural evolution re- search of Chenjiazhuang-Baimiao district in Jiyang Depression [D].Dongying:Geological Scientific Research Institute of Sin- opec Shengli Oilfield Company,2006.
[15]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 aI.Evolution of Jiyang Depression and its tectonic implications[J].Geological Journal of China Universities,1999,5(3):275-282.
[16]宗国洪，石红霞，郭元玲，等．济阳坳陷地震勘探效果分析[J]．新疆石油地质，2002，23(6)：511-512．Zong Guohong,Shi Hongxia,Guo Yuanling,et al.Analysis of seismic prospecting effectiveness in Jiyang Depression[J].Xin- jiang Petroleum Geology,2002,23(6):511-512.
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