大兴安岭地区突泉盆地高精度重磁电特征及其构造格架

doi:10.13278/j.cnki.jjuese.201601301

吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (1): 240-253.doi: 10.13278/j.cnki.jjuese.201601301

大兴安岭地区突泉盆地高精度重磁电特征及其构造格架

王丹丹^1,2, 李世臻², 周新桂², 李爱勇³, 温泉波⁴, 林燕华²

1. 中国地质大学(北京)能源学院, 北京 100083;
2. 中国地质调查局油气资源调查中心, 北京 100029;
3. 江苏省有色金属华东地质勘查局八一四队, 江苏镇江 212005;
4. 吉林大学地球科学学院, 长春 130061

收稿日期:2015-05-29 出版日期:2016-01-26 发布日期:2016-01-26
通讯作者: 李世臻(1951),男,高级工程师,主要从事石油地质和油气资源战略选区综合研究,E-mail:lishz2006@sina.com E-mail:lishz2006@sina.com
作者简介:王丹丹(1982),女,博士研究生,工程师,主要从事石油地质与综合研究工作,E-mail:ddwangcn@163.com
基金资助:
中国地质调查局项目(1211302108019-2,1212010782001)

Lithology Lithofacies Identification and Deep Structure of Tuquan Basin in Great Xinggan Range Area Based on High-Precision Gravity-Magnetic-Electrical Survey

Wang Dandan^1,2, Li Shizhen², Zhou Xingui², Li Aiyong³, Wen Quanbo⁴, Lin Yanhua²

1. School of Energy, China University of Geosciences, Beijing 100083, China;
2. Oil and Gas Survy, China Geological Survey, Beijing 100029, China;
3. Team 814, East China Bureau of Nonferrous Metals Geological Exploration, Zhenjiang 212005, Jiangsu, China;
4. College of Earth Sciences, Jilin University, Changchun 130061, China

Received:2015-05-29 Online:2016-01-26 Published:2016-01-26
Supported by:
Supported by China Geological Survey Project (1211302108019-2, 1212010782001)

摘要/Abstract

摘要：

松辽盆地西部及外围中生界是新近确定的东北油气资源新区的主力层系,其盆地内部地层展布、构造样式、油气成藏组合条件等均不明确,油气资源潜力研究程度较低。笔者以内蒙古东北部突泉盆地为主要研究区,通过高精度重力、磁力和大地电磁等地球物理方法,揭示了突泉盆地深部地层结构形态并评价油气资源潜力。综合勘探成果显示:盆地内沉积地层由盆地边缘向盆地内部逐渐倾斜,即沉积地层向盆地中心延伸,其埋深逐渐加大,马吉拉胡一带可能为盆地中心;突泉盆地内部存在区域性断裂13条,断裂走向以NE、NW向为主,这些断裂构成了研究区的基本构造格架,控制着研究区内中生界和上古生界的隆凹格局及沉积地层发育;并圈定了北部次凸、德泉次凹、白子庙次凹、东南次凸4个中生代构造单元。这些认识和成果为下一步油气资源勘探工作部署提供了盆地深部结构方面的重要证据,也对在东北油气资源新区(松辽盆地西部及外围)进行上古生界中生界油气资源潜力评价具有重要理论和现实意义。

关键词: 突泉盆地, 油气勘探, 重力, 磁力, 大地电磁(MT), 构造格架

Abstract:

In the latest round of oil and gas resources nationwide survey and integral deployment, the western district of Songliao basin and its periphery are taken as the study area to do the Mesozoic oil and gas resource potential evaluation. To gain further insight of the oil & gas resource potential of the new regions and new layers,the high precised gravity, magnetic and electrical geophysical methods are used to study the stratigraphic distribution, deep structural styles, and hydrocarbon accumulation combination of Tuquan basin. The research results indicate that the sedimentary strata gradually slopes from the edge to the centre of the basin with a gradual increase of the burial depth; 13 regional faults develop mainly in NE and NW direction in Tuquan basin, and these faults control the basic structural framework of Tuquan basin, the Mesozoic and Upper Paleozoic upwarping-downwarping pattern, as well as the sedimentary strata. We delineate four Mesozoic tectonic unites:the secondary salient of north part, the secondary depression of Dequan, the secondary depression of Baizimiao, and the secondary salient of southeast part.These perceptions and results provide important deep structure evidence of the basin for the next oil and gas exploration, and also have important theoretical and practical significance for the Upper Paleozoic-Mesozoic oil and gas resources assessment of the new oil and gas district in Northeast China(Western Songliao Basin and external area).

Key words: Tuquan basin, oil and gas exploration, gravity, magnetic, MT, tectonic framework

中图分类号:

P631

王丹丹, 李世臻, 周新桂, 李爱勇, 温泉波, 林燕华. 大兴安岭地区突泉盆地高精度重磁电特征及其构造格架[J]. 吉林大学学报(地球科学版), 2016, 46(1): 240-253.

Wang Dandan, Li Shizhen, Zhou Xingui, Li Aiyong, Wen Quanbo, Lin Yanhua. Lithology Lithofacies Identification and Deep Structure of Tuquan Basin in Great Xinggan Range Area Based on High-Precision Gravity-Magnetic-Electrical Survey[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1): 240-253.

参考文献

[1] 陈树旺,丁秋红,郑月娟,等.松辽盆地外围新区、新层系:油气基础地质调查进展与认识[J]. 地质通报,2013,32(8):1147-1158. Chen Shuwang,Ding Qiuhong,Zheng Yuejuan,et al. New Areas and Series of Strata on the Periphery of Songliao Basin:The Progress and Recognition Based on Foundational Geological Survey for Oil and Gas Resources[J]. Geological Bulletin of China,2013,32(8):1147-1158.

[2] 丁秋红,陈树旺,张立君,等. 松辽盆地外围油气新区中生代地层研究新进展[J]. 地质通报,2013, 32(8):1159-1176. Ding Qiuhong, Chen Shuwang, Zhang Lijun, et al. New Research Progress of the Mesozoic Strata in New Areas on the Periphery of Songliao Basin[J]. Geological Bulletin of China,2013,32(8):1159-1176.

[3] 方慧,钟清,陈树旺, 等.内蒙古突泉盆地双低阻层的发现及其地质意义[J]. 地质通报,2013,32(8):1253-1259. Fang Hui,Zhong Qing,Chen Shuwang,et al. The Discovery of Two Conductive Layers in Tuquan Basin, Inner Mongolia, and Its Geological Significance[J]. Geological Bulletin of China,2013,32(8):1253-1259.

[4] 刘光鼎,郝天珧,刘伊克. 重磁研究对认识盆地的意义[J].地球物理学进展,1996, 11(2):1-15. Liu Guangding, Hao Tianyao,Liu Yike. The Significance of Gravity and Magnetic Research for Knowing Sedimentary Basins[J]. Progress in Geophysics,1996,11(2):1-15.

[5] 马宗晋,高祥林,宋正范.中国布格重力异常水平梯度图判读和构造解释[J]. 地球物理学报,2006,49(1):106-114. Ma Zongjin,Gao Xianglin,Song Zhengfan. Analysis and Tectonic Interpretation to the Horizontal Gradient Map Calculated from Bouguer Gravity Data in the China Mainland[J]. Chinese Journal of Geophysics,2006, 49(1):106-114.

[6] 唐克东, 邵济安, 李永飞. 松嫩地块以及研究意义[J]. 地学前缘, 2011,18(3):57-65. Tang Kedong,Shao Ji'an,Li Yongfei. Songnen Massif and Its Research Significance[J]. Earth Science Frontiers,2011,18(3):57-65.

[7] 王杰,陈树旺,丁秋红. 内蒙古突泉盆地中侏罗统万宝组碎屑岩LA-ICP-MS锆石U-Pb测年、地球化学特征及对源区的制约[J]. 地质通报,2013, 32(8):1224-1235. Wang Jie,Chen Shuwang,Ding Qiuhong. Zircon U-Pb Dating and Geochemical Characteristics of Detrital Rocks and Their Constraints on the Provenance of Middle Jurassic Wanbao Formation in Tuquan Basin[J]. Geological Bulletin of China,2013, 32(8):1224-1235.

[8] 李永飞, 孙守亮, 郜晓勇.大兴安岭中段突泉盆地高Mg^#火山岩激光全熔⁴⁰Ar/³⁹Ar测年与地球化学特征[J]. 地质与资源, 2013,22(4):264-272. Li Yongfei,Sun Shouliang,Gao Xiaoyong. Laser ⁴⁰Ar/³⁹Ar Dating and Geochemistry of the High-Mg^# Volcanic Rocks from the Tuquan Basin in Central Daxinganling[J]. Geology and Resources,2013,22(4):264-272.

[9] 丁秋红,陈树旺,郑月娟,等. 大兴安岭地区突泉盆地侏罗系充填序列及暗色泥岩发育特征[J]. 地质与资源,2010,19(3):203-207. Ding Qiuhong,Chen Shuwang,Zheng Yuejuan,et al. The Development of Melamud Stone and the Jurassic Filling Sequence in Tuquan Basin,Daxinganling Region[J]. Geology and Resources,2010,19(3):203-207.

[10] 王五力,陈树旺,刘世伟, 等. 中国东北造山带与高原形成的关系[J]. 地质与资源,2010, 19(增刊1):39-45. Wang Wuli,Chen Shuwang,Liu Shiwei, et al. The Relationship Between Orogeny and Plateau Formation in Northeastern China[J]. Geology and Resources,2010,19(Sup.1):39-45.

[11] 李思田. 断陷盆地分析与煤聚集规律[M]. 北京:地质出版社, 1988. Li Sitian. Fault Basin Analysis and Coal Accumulation Law[M]. Beijing:Geological Publishing House,1988.

[12] 李朋武,高锐,管烨,等. 内蒙古中部索伦林西缝合带封闭时代的古地磁分析[J]. 吉林大学学报(地球科学版),2006,36(5):744-758. Li Pengwu, Gao Rui, Guan Ye, et al. Paleomagnetic Constraints on the Final Closure Time of Solonker-Linxi Suture[J]. Journal of Jilin University (Earth Science Edition), 2006,36(5):744-758.

[13] 李宁. 东北地区晚古生代地层格架[D]. 长春:吉林大学, 2011. Li Ning. Stratigraphic Framework of Late Paleozoic in Northeastern China[D]. Changchun:Jilin University,2011.

[14] 周建波, 曾维顺, 曹嘉麟, 等. 中国东北地区的构造格架与演化:从500 Ma到180 Ma[J]. 吉林大学学报(地球科学版),2012,42(5):1298-1329. Zhou Jianbo, Zeng Weishun, Cao Jialin, et al. The Tectonic Framework and Evolution of the NE China:From~500 Ma to~180 Ma[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(5):1298-1329.

[15] 陈树旺,丁秋红, 郑月娟,等. 松辽外围早侏罗世晚古生代油气远景分析[J]. 矿床地质,2010,29(增刊):1037-1038. Chen Shuwang,Ding Qiuhong,Zheng Yuejuan, et al. Early-Jurassic-Late Paleozoic Hydrocarbon Potential Analysis in the Periphery of Songliao Basin[J]. Mineral Deposits,2010, 29(Sup.):1037-1038.

[16] 蒋兴超,陈树旺,唐友军, 等. 内蒙古突泉盆地ZK-WJT钻井下侏罗统红旗组生烃潜力[J]. 地质通报,2013,32(8):1236-1242. Jiang Xingchao,Chen Shuwang,Tang Youjun,et al. The Evaluation of Hydrocarbon Production of Well ZK-WJT in Lower Jurassic Hongqi Formation Within Tuquan Basin of Inner Mongoli[J]. Geological Bulletin of China,2013, 32(8):1236-1242.

[17] 张永生, 王延斌, 卢振权, 等. 松辽盆地及外围地区石炭系二叠系烃源岩的特征[J]. 地质通报,2011, 30(2/3):214-220. Zhang Yongsheng, Wang Yanbin, Lu Zhenquan, et al. Characteristics of Source Rocks from Carboniferous-Permian in Songliao Basin and Its Peripheral Area, Northeastern China[J]. Geological Bulletin of China, 2011, 30(2/3):214-220.

[18] 钟清,方慧,李晓昌, 等. 松辽盆地外围中生代盆地的岩石物性:以突泉盆地和乌兰盖盆地为例[J]. 地质通报,2013,32(8):1185-1194. Zhong Qing,Fang Hui,Li Xiaochang,et al. Rock Physical Properties of Mesozoic Basins on the Periphery of Songliao Basin:A Case Study of Tuquan Basin and Wulangai Basin[J]. Geological Bulletin of China, 2013,32(8):1185-1194.

[19] 张交东,杨晓勇,刘成斋, 等.大别山北缘深部结构的高精度重磁电震解析[J]. 地球物理学报,2012, 55(7):2292-2306. Zhang Jiaodong,Yang Xiaoyong,Liu Chengzhai,et al. The Fine Deep Structure of the Northern Margin of the Dabie Orogenic Belt from Gravity-Magnetic-Electrical-Seismic Combination Survey[J]. Chinese Journal of Geophysics, 2012, 55(7):2292-2306.

[20] 李琴,陈立卿. 基于重磁电资料的TC盆地地层结构特征研究[J]. 石油物探,2013, 52(1):104-112. Li Qin,Chen Liqing. Study on Stratum Structure Characteristics in TC Basin by Using Gravity, Magnetic and Electric Data[J]. Geophysical Prospecting for Petroleum,2013,52(1):104-112.

[21] 时建超.鄂尔多斯南缘中新生代构造特征及演化[D].西安:西北大学, 2010. Shi Jianchao. The Mesozoic-Cenozoic Structural Characteristics and Its Evolution in Southern Ordos Region[D]. Xi'an:Northwestern University, 2010.

[22] 宋景明,金凤鸣,王玉青, 等. 二连盆地重磁异常地质意义及上古生界结构认识[J]. 石油地球物理探勘,2012, 47(增刊1):140-146. Song Jingming,Jin Fengming,Wang Yuqing,et al. Geological Implications of Gravity and Magnetic Anomalies in Erlian Basin and Understanding of Upper Paleozoic Structures[J]. Oil Geophysical Prospecting,2012, 47(Sup.1):140-146.

[23] 刘玲,张明华,田黔宁, 等. 突泉盆地磁性体重力场剥离的方法技术及岩体三维显示[J]. 物探与化探,2013, 37(2):242-245. Liu Ling,Zhang Minghua,Tian Qianning,et al. The Method of Using Gravity and Magnetic Data for Gravity Field Separating in Tuquan Basin and 3D Inversion of Rock[J]. Geophysical & Geochemical Exploration,2013,37(2):242-245.

[24] 霍光辉, 王海芹, 王仁祥, 等. 郯庐断裂带中南段重磁特征与深部构造[J]. 山东国土资源,2009, 25(8):9-13. Huo Guanghui,Wang Haiqin,Wang Renxiang,et al. Gravity and Magnetic Characteristics and Deep Structure in Middle and South Part of Tanlu Fault Belt[J]. Shandong Land and Resources,2009,25(8):9-13.

[25] 郑伟军. Tilt导数方法研究及其在重磁数据处理中的应用[D]. 北京:中国地质大学, 2010. Zheng Weijun. Research on Tilt Derivative and Application in Processing Gravity and Magnetic Data[D]. Beijing:China University of Geosciences, 2010.

[26] 赵芝. 内蒙古大石寨地区早二叠世大石寨组火山岩的地球化学特征及其构造环境[D].长春:吉林大学, 2008. Zhao Zhi. Geochenmistry and Tecgonic Setting of the Volcanin Rocks of Early Permian Dashizhai Formation in Dashizhai Area,Inner Mongolia[D]. Changchun:Jilin University, 2008.

[27] 公繁浩,黄欣,陈树旺, 等. 内蒙古西乌珠穆沁旗地区寿山沟组烃源岩有机地球化学特征[J]. 地质通报,2013,32(8):1322-1328. Gong Fanhao,Huang Xin,Chen Shuwang,et al. Organic Geochemical Characteristics of Source Rocks in Shoushangou Formation, Xiujimain Banner of Inner Mongolia[J]. Geological Bulletin of China,2013, 32(8):1322-1328.

[28] 任收麦,乔德武,张兴洲, 等. 松辽盆地及外围上古生界油气资源战略选区研究进展[J].地质通报,2011, 30(2/3):197-204. Ren Shoumai,Qiao Dewu,Zhang Xingzhou,et al. The Present Situation of Oil & Gas Resources Exploration and Strategic Selection of Potential Area in the Upper Paleozoic of Songliao Basin and Surrounding Area, NE China[J]. Geological Bulletin of China, 2011, 30(2/3):197-204.

[29] 戚良刚,王建伟,黄传杨, 等. 庐枞地区重磁场特征及其地质认识[J]. 安徽地质,2008,18(4):277-281. Qi Lianggang,Wang Jianwei,Huang Chuanyang,et al. Characteristic and Geological Understanding of Gravity, Aeromagnetic Field in Luzong Area[J]. Geology of Anhui,2008, 18(4):277-281.

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大兴安岭地区突泉盆地高精度重磁电特征及其构造格架

Lithology Lithofacies Identification and Deep Structure of Tuquan Basin in Great Xinggan Range Area Based on High-Precision Gravity-Magnetic-Electrical Survey

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