济阳坳陷车15井区浊积扇沉积及油气勘探意义
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摘要
根据岩心、地震、测录井资料,在济阳坳陷车镇凹陷车15井区的沙三下砂砾体中识别出滑塌浊积扇和深水浊积扇。其中,车古25井以具水道补给的(有根的)滑塌浊积扇为特色;内扇及水道最发育,为碎屑流夹浊流的巨砾岩、中细砾岩(厚10～20 m)与砾质砂岩夹薄层深灰、灰色泥岩;崩塌成因的巨砾(大小1.06 m)反映了陡的斜坡;地震上呈楔状外形,内扇为弱反射,中扇与外扇为发散、亚平行的连续反射。车57井以粒度偏细且有根的深水浊积扇与深湖相互层为特色;中扇发育,为厚(5～11 m)的水道碎屑流细砾岩与砾质砂岩,夹深灰色泥岩;水道沉积表现为钟型测井曲线。顺水道方向滑塌浊积扇由北而南产生进积,向盆出现深水浊积扇;2类扇体沿主构造线串珠状排列,包裹于大片的深湖相中,呈现"深湖包扇"的沉积格局。不同类型浊积扇的识别及其边界的确定,对于该区隐蔽圈闭勘探具有重要意义。
Based on seismic,well-logging and core data,the authors recognized the deep-water turbidity fans and slide turbidity fans developed in the lower 3rd Member of Shahejie Formation from the well block Che 15 in Chezhen sag,Jiyang depression.Well Chegu 25 is characterized by the slide turbidity fans with supplied or rooted channels,where the inner fan and its channels are especially developed,and are composed of debris-flow and a few turbidity-flow boulder-,cobble-and pebble-conglomerates with thickness of 10 to 20 m and gravel sandstones bedded with thin-layer dark grey or grey mudstones;the conglomerates of falling-boulder 1.06m in size reflect steep slope topography.On the seismic profiles,the fans assume wedge form,where the inner-fan is weakly reflected,and the middle-and outer-fans are of divergently and subparallelly continuous seismic reflection configuration.Well Che 57 of fine-grained sediments is characterized by the deep-water turbidity fans with rooted channels and deep lacustrine facies,where the middle-fans are especially developed,and are composed of debris-flow pebbly-conglomerates with thickness of 5 to 11m and gravel sandstones interlayered with dark grey mudstones;the well-logging curve pattern of channel sediments is bell-shaped.it is concluded that the slide turbidity fans experienced progradation along the channels from north to south,and the deep-water turbidity fans occurred in the central lake;two types of fans were disposed in the pinch-and-swell form along the main tectonic orientation,and were wrapped in extensively-distributed deep lake facies,assuming the sedimentary framework of "fans packaged in deep-lake".The recognition and confirmation of boundaries of the turbidity fans is of great significance for hydrocarbon prospecting of the subtle traps.
Based on seismic,well-logging and core data,the authors recognized the deep-water turbidity fans and slide turbidity fans developed in the lower 3rd Member of Shahejie Formation from the well block Che 15 in Chezhen sag,Jiyang depression.Well Chegu 25 is characterized by the slide turbidity fans with supplied or rooted channels,where the inner fan and its channels are especially developed,and are composed of debris-flow and a few turbidity-flow boulder-,cobble-and pebble-conglomerates with thickness of 10 to 20 m and gravel sandstones bedded with thin-layer dark grey or grey mudstones;the conglomerates of falling-boulder 1.06m in size reflect steep slope topography.On the seismic profiles,the fans assume wedge form,where the inner-fan is weakly reflected,and the middle-and outer-fans are of divergently and subparallelly continuous seismic reflection configuration.Well Che 57 of fine-grained sediments is characterized by the deep-water turbidity fans with rooted channels and deep lacustrine facies,where the middle-fans are especially developed,and are composed of debris-flow pebbly-conglomerates with thickness of 5 to 11m and gravel sandstones interlayered with dark grey mudstones;the well-logging curve pattern of channel sediments is bell-shaped.it is concluded that the slide turbidity fans experienced progradation along the channels from north to south,and the deep-water turbidity fans occurred in the central lake;two types of fans were disposed in the pinch-and-swell form along the main tectonic orientation,and were wrapped in extensively-distributed deep lake facies,assuming the sedimentary framework of "fans packaged in deep-lake".The recognition and confirmation of boundaries of the turbidity fans is of great significance for hydrocarbon prospecting of the subtle traps.
引文
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[2]范振峰.车西洼陷北带湖底扇成因机制及其勘探意义[J].新疆石油地质,2007,28(1):48-50.Fan Zhenfeng.The origin of sublacustrine fan and its significancefor exploration in Northern Chexi Sub-Sag,Jiyang Depression[J].Xinjiang Petroleum Geology,2007,28(1):48-50(in Chinese withEnglish abstract).
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[4]孟万斌,张善文,田波,等.沾化凹陷五号桩地区沙河街组三段浊流沉积特征及储集性能[J].石油与天然气地质,2007,28(4):504-510.Meng Wanbin,Zhang Shanwen,Tian Bo,et al.Depositionalcharacteristics and reservoir properties of turbidites in the 3~(rd)member of Shahejie Formation in Wuhaozhuang area,easternZhanhua depression[J].Oil&Gas Geology,2007,28(4):504-510(in Chinese with English abstract).
[5]Li Pilong,Zhang Shanwen,Xiao Huanqin,et al.Exploration ofsubtle trap in Jiyang Depression[J].Petroleum Science,2004,1(2):13-21.
[6]刘传虎.砂砾岩扇体发育特征及地震描述技术[J].石油物探,2001,40(1):64-72.Liu Chuanhu.Features and seismic description of glutenite segment[J].Geophysical Prospecting for Petroleum,2001,40(1):64-72(inChinese with English abstract).
[7]袁静.济阳坳陷南部古近系洪水—漫湖沉积[J].中国地质,2005,32(4):655-662.Yuan Jing.Paleogene flooded lake sediments in the southern part ofthe Jiyang depression[J].Geology in China,2005,32(4):655-662(in Chinese with English abstract).
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[9]韦东晓,田景春,倪新锋.湖相浊积砂体沉积特征及油气勘探意义[J].油气地质与采收率,2006,13(5):15-17.Wei Dongxiao,Tian Jingchun,Ni Xinfeng.Sedimengtarycharacteristics of lacustrine turbidite sand body and its significanceson petroleum exploration[J].Petroleum Geology and RecoveryEfficiency,2006,13(5):15-17(in Chinese with English abstract).
[10]张萌,田景春.“近岸水下扇”的命名、特征及其储集性[J].岩相古地理,1999,19(4):42-52.Zhang Meng,Tian Jingchu.The nomenclature,sedimentarycharacteristics and Reservoir potential of nearshore subaqueous fan[J].Sedimentary Facies and Palaeogeography,1999,19(4):42-52(inChinese with English abstract).
[11]李丕龙,张善文,宋国奇,等.济阳成熟探区非构造油气藏深化勘探[J].石油学报,2003,24(5):10-15.Li Pilong,Zhang Shanwen,Song Guoqi,et al.Explorationpotential of nonstructural pools in the matured acreage of JiyangDistrict[J].Acta Petrolei Sinica,2003,24(5):10-15(in Chinesewith English abstract).
[12]王永诗,鲜本忠.车镇凹陷北部陡坡带断裂结构及其对沉积和成藏的控制[J].油气地质与采收率,2006.13(6):5-8.Wang Yongshi,Xiang Benzhong.Fault structures of northern steepbelts and their influences on sedimentation and reservoir formationin Chezhen Sag[J].Petroleum Geology and Recovery Efficiency,2006.13(6):5-8(in Chinese with English abstract).
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[14]彭勇民,黄捍东,罗群.济阳坳陷车镇凹陷车66块沙三下段精细沉积相分析[J].现代地质,2007,27(4):18-23.Peng Yongmin,Huang Handong,Luo Qun.Fine analysis ofsedimentary facies in the Lower Third Member of ShahejieFormation from Block Che 66 in Chezhen Sag,Jiyang Depression[J].Geoscience,2007,27(4):18-23(in Chinese with Englishabstract)
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[17]施振生,朱筱敏,胡斌,等.济阳坳陷车镇凹陷古近系沙河街组遗迹化石Maca ronichnus(通心粉管迹)及其沉积环境[J].古地理学报,2004,16(12):207-215.Shi Zhensheng,Zhu Xiaomin,Hu Bin,et al.Sedimentaryenvironments of Maca ronichnus of the Shahejie Formation ofPaleogene of Chezhen Sag in Jiyang Depression[J].Journal ofPalaeogeography,2004,16(12):207-215(in Chinese with Englishabstract).
[18]张家震,毕彩芹,王新峰,等.车镇凹陷石油地质特征及勘探远景[J].海洋石油,2005,26(3):6-10.Zhang Jiazhen,Bi Caiqin,Wang Xinfeng,et al.Petroleum and oilgeology and exploratory prospect of Chezhen Sag[J].OceanGeology,2005,26(3):6-10(in Chinese with English abstract).
[19]朱光有,金强,张水昌,等.车镇凹陷下第三系沙河街组生烃系统研究[J].天然气工业,2006,26(3):19-22.Zhu Guangyou,Jin Qiang,Zhang Shuichang,et al.Hydrocarbongenerating system of Eogene Shahejie Fm in Chezhen sag[J].Natural Gas in Dustry,2006,26(3):19-22(in Chinese withEnglish abstract).
[20]陈清华,王秀玲.陆相断陷盆地“五扇一沟”的地震响应特征[J].特种油气藏,2007,14(1):15-19.Chen Qinghua,Wang Xiuling.Seismic characteristics of“five-fanone-channel turbidite”in continental rift basin[J].Special Oil and GasReservoirs,2007,14(1):15-19(in Chinese with English abstract).
[21]刘宪斌,万晓樵,林金逞,等.陆相浊流沉积体系与油气[J].地球学报,2003,24(1):61-66.Liu Xianbin,Wan Xiaoqiao,Lin Jincheng,et al.Continentalturbidite deposition system and hydrocarbon[J].Acta GeosicientiaSinica,2003,24(1):61-66(in Chinese with English abstract).
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