The application of constrained sparse spike impedance inversion to seismic exploration of land gas hydrate
WANG Kai1, 2, 3, CHEN De-Yuan1, 2, ZHANG Kai1, 2, YUE Hang-Yu1, 2, ZHANG Bao-Wei1, 2, WANG Xiao-Jiang1, 2
1.Institute of Geophysical and Geochemical Exploration,CAGS,Langfang 065000,China; 2.National Modern Geological Exploration Technology Research Center,Langfang 065000,China; 3.College of GeoExploration Science and Technology,Jilin University,Changchun 130026,China
Abstract:Natural gas hydrates are mainly distributed below the seabed and in the permafrost zones.There are obvious characteristics for the impedance of the sea gas hydrate.Nevertheless,very insufficient research has been focused on the impedance characteristics of the land gas hydrate.In this paper,the research aimed at the land gas hydrate in Muli area of the Tibetan Plateau.The authors used the constrained sparse-spike method to invert the impedance with 2D reflected seismic profile which crossed the DK-9 well.The authors analyzed the features of the impedance profile of the four layers that contain gas hydrate.The results show that the impedance of land gas hydrate reservoir is on the whole the same as things of the surroundings.There are a lot of difficulties in detecting the land gas hydrate with wave impedance individually,and hence the reservoir should be detected in combination with other geological and geophysical data.
王凯, 陈德元, 张凯, 岳航羽, 张保卫, 王小江. 青海木里地区陆域天然气水合物地震波阻抗特征研究[J]. 物探与化探, 2017, 41(6): 1105-1112.
WANG Kai, CHEN De-Yuan, ZHANG Kai, YUE Hang-Yu, ZHANG Bao-Wei, WANG Xiao-Jiang. The application of constrained sparse spike impedance inversion to seismic exploration of land gas hydrate. Geophysical and Geochemical Exploration, 2017, 41(6): 1105-1112.
[1] Paull C K,Dillon W P.Natural gas hydrate:Occurrence,distribution,and detection[J].American Geophysical Union Geophysical Monograph,2001,124:3-18. [2] Sloan E D,Koh C A.Clathrate hydrates of natural gases(3 rd ed)[M].New York:CRC press,2008. [3] 杨睿,吴能友,雷新华,等.波阻抗反演在南海北部神狐海域天然气水合物勘探中的应用[J].现代地质,2010,24(3):495-500. [4] Michael R,Bellefleur G,Mair S,et al.Acoustic impedance inversion and seismic reflection continuity analysis for delineating gas hydrate resources near the Mallik research sites,Mackenzie Delta,Northwest Territories,Canada[J].Geophysics,2009,74(5):B125-B137. [5] 曹代勇,刘天绩,王丹,等.青海木里地区天然气水合物形成条件分析[J].中国煤炭地质,2009,21(9):3-6. [6] 徐明才,刘建勋,张保卫,等.陆域天然气水合物地震探测有效性试验研究[J].物探化探计算技术,2013,35(4):375-381. [7] 徐明才,刘建勋,柴明涛,等.青海省天峻县木里地区天然气水合物地震响应特征[J].地质通报,2011,30(12):1910-1917. [8] 徐明才,刘建勋,柴铭涛,等.青海木里地区天然气水合物反射地震试验研究[J].地质与勘探,2012,48(6):1180-1187. [9] 纱志彬,郑涛,杨木壮,等.基于波阻抗反演的天然气水合物地震检测技术[J].现代地质,2010,24(3):481-488. [10] Shaoming Lu G a M.Elastic impedance inversion of multichannel seismic data from unconsolidated sediments containing gas hydrate and free gas[J].Geophysics,2004,69(1):164-179. [11] 薛花,张宝金,徐云霞,等.波阻抗反演在琼东南海域水合物检测中的应用[J].海洋地质与第四纪地质,2016,36(2):173-180. [12] 金春爽,乔德武,卢振权,等.青海木里冻土区水合物稳定带的特征研究-模拟结果与钻探结果对比[J].地球物理学报,2011,54(1):173-181. [13] 文怀军,鲁静,尚潞君,等.青海聚乎更矿区侏罗纪含煤岩系层序地层研究[J].中国煤田地质,2006,18(5):19-21. [14] 侯颉,邹长春,曲璐,等.青海木里三露天天然气水合物储层测井识别与划分[J].现代地质,2015,29(5):1110-1121. [15] 郭星旺,祝有海.祁连山冻土区DK-1钻孔天然气水合物测井响应特征和评价[J].地质通报,2011,30(12):1868-1873. [16] 刘杰,刘江平,程飞,等.基于岩石物理方法分析青藏高原天然气水合物填充模式[J].天然气地球科学,2015,26(11):2198-2207. [17] 许永忠,杨海军.地震反演技术在岩性及火成岩识别中的研究与应用[M].徐州:中国矿业大学出版社,2012. [18] 黄绪德.反褶积与地震道反演[M].北京:石油工业出版社,1992. [19] 栾颖.约束稀疏脉冲波阻抗反演方法在煤层识别中的应用[D].长春:吉林大学,2010.