吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (2): 517-524.doi: 10.13278/j.cnki.jjuese.20170269
姚刚1, 董向欣2, 李丽丽2, 马国庆2, 孟令顺2
Yao Gang1, Dong Xiangxin2, Li Lili2, Ma Guoqing2, Meng Lingshun2
摘要： 本文利用面积广、勘探深度大的重磁数据通过增强型局部相位边界识别方法和优化欧拉反褶积法获得东海陆架盆地的构造特征，为油气勘探提供基础资料。增强型局部相位边界识别法是重磁数据一阶和二阶水平导数的比值函数，能有效地均衡不同深度地质体的边界响应，从而同时显示不同深度构造的边界，提高对较深层构造的分辨率；优化欧拉反褶积法有效地降低了背景异常的干扰，从而可获得更加准确的构造反演结果。理论模型研究表明，增强型局部相位边界识别法可更加准确和清晰地划分边界信息，优化欧拉反褶积法可获得更加准确和收敛的反演结果。综合利用增强型局部相位边界识别和优化欧拉反褶积法对东海陆架断裂构造分布进行划分，获得了分析区域构造背景和评估油气潜力的基础资料。
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| [1] Cooper G R J, Cowan D R. Enhancing Potential Field Data Using Filters Based on the Local Phase[J]. Computers & Geosciences, 2006, 32(1):1585-1591. [2] Cooper G R J, Cowan D R. Edge Enhancement of Potential-Field Data Using Normalized Statistics[J]. Geophysics, 2008, 73(3):H1-H4. [3] Ma G. EdgeDetection of Potential Field Data Using Improved Local Phase Filter[J]. Exploration Geophysics, 2013, 44(1):36-41. [4] Miller H G, Singh V. Potential Field Tilt:A New Concept for Location of Potential Field Sources[J]. Journal of Applied Geophysics, 1994, 32:213-217. [5] Roest W R, Verhoef J, Pilkington M. Magnetic Interpretation Using the 3-D Analytic Signal[J]. Geophysics, 1992, 57:116-125. [6] Wijns C, Perez C, Kowalczyk P. Theta Map:Edge Detection in Magnetic Data[J]. Geophysics, 2005, 70(4):L39-L43. [7] Thompson D T. EULDPH:A New Technique for Making Computer:Assisted Depth Estimates from Magnetic Data[J]. Geophysics, 1982, 47(1):31-37. [8] Reid A N, Allsop J M, Granser H, et al. Magnetic Interpretation in Three Dimensions Using Euler Deconvolution[J]. Geophysics, 1990, 55(1):80-91. [9] 刘申叔,李上卿.东海油气地球物理勘探[M].北京:地质出版社,2001. Liu Shenshu, Li Shangqing. Geophysical Exploration of Oil and Gas in the East China Sea[M]. Beijing:Geological Publishing House, 2001. [10] 骆满生,卢隆桥,贾建,等.中国中生代沉积盆地演化[J].地球科学:中国地质大学学报,2014,39(8):954-976. Luo Mansheng, Lu Longqiao, Jia Jian, et al. Evolution of Sedimentary Basins in China During Mesozoic[J]. Earth Science:Journal of China University of Geosciences, 2014, 39(8):954-976. [11] 张岳桥,徐先兵,贾东,等.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录[J]地学前缘,2009,16(1):234-247. Zhang Yueqiao, Xu Xianbing, Jia Dong, et al. Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China During the Early Mesozoic[J]. Earth Science Frontiers, 2009, 16(1):234-247. [12] 李益龙,周汉文,肖文交,等.古亚洲构造域和西太平洋构造域在索伦缝合带东段的叠加:来自内蒙古林西县西拉木伦断裂带内变形闪长岩的岩石学、地球化学和年代学证据[J].地球科学:中国地质大学学报,2012,37(3):433-450. Li Yilong, Zhou Hanwen, Xiao Wenjiao, et al. Superposition of Paleo-Asian and West-Pacific Tectonic Domains in the Eastern Section of the Solonker Suture Zone:Insights from Petrology, Geochemistry and Geochronology of Deformed Dioritein Xar Moron Fault Zone, Inner Mongolia[J]. Earth Science:Journal of China University of Geosciences, 2012, 37(3):433-450. [13] 李三忠,张国伟,周立宏,等.中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲[J].地学前缘,2011,18(3):79-107. Li Sanzhong, Zhang Guowei, Zhou Lihong, et al. The Opposite Meso-Cenozoic Intracontinental Deformations Under the Superconvergence:Rifting and Extension in the North China Cratonand Shortening and Thrusting in the South China Craton[J]. Earth Science Frontiers, 2011, 18(3):79-107. [14] Richards M A. Lithgow-Bertelloni C Plate Motion Changes the Hawaiian-Emperor Bend and the Apparent Success and Failure of Geodynamic Models[J]. Earth and Planetary Science Letters, 1996, 137(1/2/3/4):19-27. [15] 徐亚东,梁银平,江尚松,等.中国东部新生代沉积盆地演化[J].地球科学:中国地质大学学报,2014,39(8):1079-1098. Xu Yadong, Liang Yinping, Jiang Shangsong, et al. Evolution of Cenozoic Sedimentary Basins in Eastern China[J]. Earth Science:Journal of China University of Geosciences, 2014, 39(8):1079-1098. [16] 王力锋,汪集旸.东海天然气水合物地热研究及其环境意义[J].地学前缘,2006,13(1):15-20. Wang Lifeng, Wang Jiyang. A Geothermal Study of Gas Hydrates in the East China Sea and Its Environmental Implications[J]. Earth Science Frontiers, 2006, 13(1):15-20. [17] 龚建明,李刚,杨传胜,等. 东海陆架盆地南部中生界分布特征与油气勘探前景[J].吉林大学学报(地球科学版),2013,43(1):20-27. Gong Jianming, Li Gang, Yang Chuansheng, et al. Hydrocarbon Prospecting of Mesozoic Strata in Southern East China Sea Shelf Basin[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(1):20-27. |
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