Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (5): 1522-1531.doi: 10.13278/j.cnki.jjuese.20170129

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Integrated Geophysical Exploration of Volcanic Edifice of Hengtoushan Volcano, Yitong Basin

Wang Kun1,2, Zeng Zhaofa1,2, Zhang Lianghuai3, Li Jing1,2, Lu Qi1,2, Zhang Jianmin1,2   

  1. 1. College of GeoExploration Science and Technology, Jilin University, Changchun 130026, China;
    2. Key Laboratory of Applied Geophysics, Ministry of Land and Resources of PRC, Changchun 130026, China;
    3. Jilin Earthquake Administration, Changchun 130022, China
  • Received:2018-01-08 Published:2018-11-20
  • Supported by:
    Supported by National Key Research and Development Program of China (2016YFC060110402) and National Natural Science Foundation of China(41504083)

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Abstract: The Yitong basin is a Cenozoic fault basin in the northern part of the Tan-Lu fault zone. The development and evolution of the Yitong basin is accompanied by strong volcanic activity. The distribution of buried volcanic edifices is of great significance to the study of volcanic evolution, geothermal exploration, and development in Yitong basin. In this study, we took the Hengtoushan volcano in the Yitong volcanic group as the research object, and used aeromagnetic measurements to determine the plane range of the buried volcanic edifice. The magnetic anomaly of the Hengtoushan volcanic area ranges of 2.6 km2. Using an electromagnetic sounding (MT) section through the Hengtoushan volcanic area, we obtained the deep electrical structure, and analyzed the cause of the Hengtoushan volcano. The study shows that the volcanic strata formed in the first part of the Quaternary in Early Pleistocene, and under the action of torsional stress the basaltic magma crushed out of the surface along the Maanshan fault or stuck in the fault. Now, the magma channel is closed. Using the controllable source audio magneto telluric sounding method, the fine electrical structure near the Hengtoushan volcano was obtained to determine the shape and distribution range of the concealed magma capsule. Based on the above results, we obtained a clear understanding of the formation time, deep dynamic process, the spatial morphology, and the tectonic environment of the Hengtoushan volcano. We established a geophysical imaging mechanism for a buried volcanic edifice, which provides a reference for the development of volcanic geothermal systems in the Yitong basin.

Key words: Yitong volcanoes, Hengtoushan volcano, volcanic edifice, geophysical prospecting

CLC Number: 

  • P631
[1] 陈墨香, 汪集旸, 邓孝. 中国地热系统类型图及其简要说明[J]. 地质科学, 1996,31(2):5-10. Chen Moxiang, Wang Jichang, Deng Xiao. The Map of Geothermal Ssytem Types in China and Its Brief Explanation[J]. Scientia Geologica Sinica, 1996,31(2):5-10.
[2] Byrdina S, Friedel S, Vandemeulebrouck J, et al. Geo-physical Image of the Hydrothermal System of Merapi Volcano[J]. Journal of Volcanology & Geothermal Research, 2017,329:30-40.
[3] Portal A, Gailler L S, Labazuy P, et al. Geophysical Imaging of the Inner Structure of a Lava Dome and Its Environment Through Gravimetry and Magnetism[J]. Journal of Volcanology & Geothermal Research, 2016, 320:88-99.
[4] Okubo A, Nakatsuka T, Tanaka Y. Aeromagnetic Constraits on the Subsurface Structure of the Unzen Graben, Kyushu, Japan[J]. Earth, Planets and Space, 2006, 58(1):23-31.
[5] 汤吉, 王继军, 陈小斌,等.阿尔山火山区地壳上地幔电性结构初探[J].地球物理学报,2005, 48(1):196-202. Tang Ji, Wang Jijun, Chen Xiaobin, et al. Preliminary Investigation for Electric Conductivity Structure of the Crust and Upper Mantle Beneath the Aershan Volcano Area[J]. Chinese Journal of Geophysics, 2005, 48(1):196-202.
[6] Savin C, Ritz M, Join J L, et al. Hydrothermal Sy-stem Mapped by CSAMT on Karthala Volcano, Grande Comore Island, Indian Ocean[J]. Journal of Applied Geophysics, 2001, 48(3):143-152.
[7] 姜梓萌. 长白山地区地热资源综合地球物理研究[D]. 长春:吉林大学, 2013. Jiang Zimeng. The Study of Integrated Geophysics for Geothermal Resources Exploration in Changbai Mountain[D]. Changchun:Jilin university, 2013.
[8] 李胜涛, 张森琦, 贾小丰,等. 五大连池尾山地区存在干热岩资源的可能性探讨[J]. 科技导报, 2016, 34(5):67-73. Li Shengtao, Zhang Senqi, Jia Xiaofeng, et al. Possibility of Hot Dry Rock Resources in Weishan Volcano Area of Wudalianchi[J]. Science and Technology Review, 2016, 34(5):67-73.
[9] 付长亮,孙德有,魏红艳,等. 伊通新生代玄武岩地球化学成分差异性研究[J]. 吉林大学学报(地球科学版),2009,39(3):446-454. Fu Changliang, Sun Deyou, Wei Hongyan, et al. Research on the Geochemical Difference of the Cenozoic Basalts in Yitong Area[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(3):446-454.
[10] 王振中. 吉林省伊通火山群[J]. 吉林地质, 1994,13(2):29-35. Wang Zhenzhong. The Yitong Volcanic Cluster of Jilin Province[J]. Jilin Geology, 1994, 13(2):29-35.
[11] 张宝政, 刘玉海. 佳木斯-伊通断裂带的基本特征及其与郯庐断裂带的关系[J]. 吉林大学学报(地球科学版), 1982, 12(1):29-39. Zhang Baozheng, Liu Yuhai. The Main Characters of Jiamusi-Yitong Fracture Belt and Its Relationship tothe Tan-Lu Fracture Belt[J]. Journal of Jilin University (Earth Science Edition), 1982,12(1):29-39.
[12] 唐大卿, 陈红汉, 孙家振,等. 郯庐断裂带伊通段新生代构造演化特征及其控盆机制[J]. 大地构造与成矿学, 2010, 34(3):340-348. Tang Daqing, Chen Honghan, Sun Jiazhen, et al. Cenozoic Tectonic Evolution of the Yitong Part of the Tan-Lu Fault Zone and Its Control on Yitong Basin[J]. Geotectonica Et Metallogenia, 2010, 34(3):340-348.
[13] 唐大卿, 何生, 陈红汉,等. 伊通盆地断裂体系特征及其演化历史[J]. 吉林大学学报(地球科学版), 2009, 39(3):386-396. Tang Daqing, He Sheng, Chen Honghan, et al. Fault System's Characteristics of Yitong Basin and Its Evolution[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(3):386-396.
[14] 唐大卿. 伊通盆地构造特征与构造演化[D]. 武汉:中国地质大学, 2009. Tang Daqing. The Structural Character and Tectonic Evolution of Yitong Basin[D]. Wuhan:China University of Geosciences,2009.
[15] 刘嘉麒. 中国东北地区新生代火山幕[J]. 岩石学报, 1988, 4(1):3-12. Liu Jiaqi. The Cenozoic Volcanoes in Northeastern China[J]. Acta Petrologica Sinica, 1988, 4(1):3-12.
[16] 张良怀,章振铨,李志田. 吉林省新生代火山活动的基本特点及其与构造活动的关系[J]. 东北地震研究,1990,6(1):101-109. Zhang Lianghuai, Zhang Zhenquan, Li Zhitian. Cenozoic Volcanism in Jilin Province and Relative Tectonism[J]. Northeast Seismological Research, 1990, 6(1):101-109.
[17] 周俊法, 吴江涛. 航磁异常与陆相火山机构[J]. 地质与勘探, 1983(1):51-58. Zhou Junfa, Wu Jiangtao. Aeromagnetic Anomalies and Continental Volcanic Institutions[J]. Geology and Exploration, 1983(1):51-58.
[18] 汤吉,詹艳,赵国泽,等. 青藏高原东北缘玛沁-兰州-靖边剖面地壳上地幔电性结构研究[J].地球物理学报, 2005,48(5):1205-1216. Tang Ji, Zhan Yan, Zhao Guoze, et al. Electrical Conductivity Structure of the Crust and Upper Mantle Along the Profile Maqin-Lanzhou-Jingbian in the Northeastern Margin of the Qinghai-Tibet Plateau[J]. Chinese Journal of Geophysics, 2005, 48(5):1205-1216.
[19] Rodi W, Mackie R L. Nonlinear Conjugate Gradients Algorithm for 2-D Magnetotelluric Inversion[J]. Geophysics, 2012, 66(1):174-187.
[20] 韩作振,宋志刚, 高丽华, 等. 吉林省"大黑山条垒带"晚古生代火山事件及其构造意义[J]. 地学前缘, 2017, 24(2):186-201. Han Zuozhen, Song Zhigang, Gao Lihua, et al. Late Paleozoic Volcanic Events in "Daheishan Horst" in Jilin, China and Their Tectonic Significance[J]. Earth Science Frontiers,2017, 24(2):186-201.
[21] Tang Y, Obayashi M, Niu F, et al. Changbaishan Volcanism in Northeast China Linked to Subduction-Induced Mantle Upwelling[J]. Nature Geoscience, 2014, 7(6):470-475.
[22] Pei S, Chen Y J. Tomographic Structure of East Asia:I:No Fast (Slab) Anomalies Beneath 660 km Discontinuity[J]. Earthquake Science, 2010, 23(6):597-611.
[23] 刘祥,向天元.中国东北地区新生代火山和火山碎屑堆积物资源与灾害[M]. 长春:吉林大学出版社, 1996. Liu Xiang, Xiang Tianyuan. Cenozoic Volcanoes and Pyroclastic Deposits in Northeastern China:Resources and Hazards[M]. Changchun:Publishing House of Jilin University, 1996.
[24] 刘茂强, 杨丙中. 伊通-舒兰地堑地质构造特征及其演化[M]. 北京:地质出版社, 1993. Liu Maoqiang, Yang Bingzhong. Geological Tectonic Features and Evolution of Yitong-Shulan Graben[M]. Beijing:Geological Publishing House, 1993.
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