Please wait a minute...
E-mail Alert Rss
 
物探与化探  2015, Vol. 39 Issue (2): 253-261    DOI: 10.11720/wtyht.2015.2.07
  资源勘查 本期目录 | 过刊浏览 | 高级检索 |
地热资源地震勘探方法综述
王丹1, 魏水建1, 贾跃玮1, 卢志2
1. 中石化石油勘探开发研究院, 北京 100083;
2. 中石油辽河油田勘探开发研究院, 辽宁 盘锦 124010
An overview of methods for geothermal seismic exploration
WANG Dan1, WEI Shui-Jian1, JIA Yue-Wei1, LU Zhi2
1. Petroleum Exploration and Production Research Institute of Sinopec, Beijing 100083, China;
2. Exploration and Development Research Institute, Liaohe Oilfield Branch Company of PetroChina, Panjin 124010, China
全文: PDF(2909 KB)   HTML
输出: BibTeX | EndNote (RIS)      
摘要 

全球地热资源丰富,具有巨大的开发潜力,它将在全球的经济发展中起到强大的推动作用。地震方法是高精度地热勘探开发中不可或缺的手段。地热资源地震勘探方法包括主动地震和被动地震两大类,这两类地震方法在地热勘探的不同阶段各自发挥着重要作用。首先分析了地热储层的地震响应特征,然后总结了国内外被动地震和主动地震勘探新技术,为进一步提高我国的地热资源地震勘探水平提供一些借鉴。研究表明,被动地震在地热田最初的普查中起到关键作用,但是在地热储层特征的精细刻画和裂缝探测的预测精度方面,该方法存在一定的缺陷;主动方法虽然成本相对较高,但是由于其高信噪比和高分辨率,所以它能更好地描述储层特征,为未开发地热区选区评价和井位优选提供可靠的技术保障;此外,多波技术也将是地热勘探未来发展的重要方向。

服务
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章
Abstract

Geothermal resources are very abundant in the world and thus have great exploration potential.In addition,the geothermal resources will considerably stimulate the global economic development.In the exploration and development of geothermal resources,the seismic technique has been playing the essential role.This technique mainly includes active and passive seismic methods which are to be conducted at different stages of geothermal exploration.In this paper,seismic responses of geothermal reservoir are analyzed first,then new technologies of passive and active seismic methods are summarized,with the purpose of providing some valuable references for the geothermal seismic exploration in China.Studies show that passive seismic method should be conducted first in the initial geothermal survey.Nevettheless,this method has some limitations on the precision in the fracture detection and the description of permeability features;in contrast,active seismic method,which relies on the high S/N ratio and high-resolution itself, can describe reservoir characteristics better,therefore guaranteeing more-refined regional evaluation and extreme site optimization of undeveloped geothermal areas.Besides,multi-wave technique also will be the future orientation of geothermal development.

收稿日期: 2014-01-20      出版日期: 2015-04-10
:  P631.4  
基金资助:

国家重大专项(2011ZX05005-002-003-003);中石化科技部项目(P12109)

作者简介: 王丹(1987-),女,助理工程师。2012年毕业于中国石油大学(北京)地球探测与信息技术专业,获硕士学位。现在中国石化石油勘探开发研究院从事储层预测研究工作。
引用本文:   
王丹, 魏水建, 贾跃玮, 卢志. 地热资源地震勘探方法综述[J]. 物探与化探, 2015, 39(2): 253-261.
WANG Dan, WEI Shui-Jian, JIA Yue-Wei, LU Zhi. An overview of methods for geothermal seismic exploration. Geophysical and Geochemical Exploration, 2015, 39(2): 253-261.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2015.2.07      或      https://www.wutanyuhuatan.com/CN/Y2015/V39/I2/253

[1] Birol F,Olerjarnik P.Will China lead the world into a clean-energy future[J].Economics of Energy and Environmental Policy,2012,1(1):5-9.

[2] 蔺文静,刘志明,王婉丽,等.中国地热资源及其潜力评估[J].中国地质,2013,40(1):312-321.

[3] 陈 煊,李德春,须振华.地震勘探技术在地热勘探中的应用[J].工程勘察,2008,(12):57-59.

[4] 刘革,刘迪新.地震方法在地热勘探中的应用[J].煤炭技术,2002,21(4):113-117.

[5] 孙党生,雷炜,李洪涛,等.高分辨率地震勘探在地热资源勘查中的应用[J].勘察科学技术,2002,6:55-59.

[6] 曾昭发,陈雄,李静,等.地热地球物理勘探新进展[J].地球物理学进展,2012,27 (1):168-178.

[7] Jaya M S,Shapiro S A,Kristinsdóttir L H,et al.Temperature dependence of seismic properties in geothermal rocks at reservoir conditions[J].Geothermics,2010,39(1):115-123.

[8] Panea I,Negut A,Mocanu V.The relationship between the deep faults and the geothermal structures identified on the Moesian Platform territory//presented at the 2011 SEG Annual Meeting, 2011.

[9] 周厚芳,刘闯,石昆法.地热资源探测方法研究进展[J].地球物理学进展,2003,18(4):656-661.

[10] Karastathis V K,Papoulia J,Fiore B D,et al.Deep structure investigations of the geothermal field of the North Euboean Gulf,Greece,using 3-D local earthquake tomography and Curie Point Depth analysis[J].J Volcanol Geoth Res,2011,206(3):106-120.

[11] Matteis R D,Vanorio T,Zollo A,et al.Three-dimensional tomography and rock properties of the Larderello-Travale geothermal area,Italy[J].Phys Earth Planet In,2008,168(1):37-38.

[12] Xu P F,Li C J,Ling S Q.Mapping collapsed columns in coal mines utilizing microtremor survey methods[J].Chinese J Geophys,2009,52(7):1923-1930.

[13] Shapiro N M,Campillo M,Stehly L,et al.High-resolution surface-wave tomography from ambient seismic noise[J].Science,2005,307(5715):1615-1618.

[14] Sabra K G,Gerstoft P,Roux P,et al.Surface wave tomography from microseisms in Southern California[J].Geophys Res Lett,2005,32 (14):L14311.

[15] Toks Z M N,Lacoss R T.Microseisms:Mode structure and sources[J].Science,1968,159(3817):872-873.

[16] Ling S Q.Research on the estimation of phase velocities of surface waves in microtremors.Hokkaido University,1994.

[17] Okada H.Theory of efficient array observations of microtremors with special reference to the SPAC method[J].Exploration Geophysics,2006,37(1):73-85.

[18] Yang M,Elkibbi M,Rial J A.An inversion scheme to model subsurface fracture systems using shear wave splitting polarization and delay time observations simultaneously[J].Geophys J Int,2005,160(3):939-942.

[19] Xu P F,Ling S,Zhang D M,et al.Geothermal exploration and exploitation using microtremor survey method:methodology and examples//Denver:2010 SEG Annual Meeting,2010.

[20] Toksοz M N,Zhang H J,Li J L.Geothermal reservoir characterization using passive seismic tomography:A case history//The Istanbul 2012-International Geophysical Conference and Oil & Gas Exhibition,2012.

[21] Reiter D,Leidig M,Ferris A,et al.Improved time-dependent seismic monitoring systems for shallow reservoir characterization[J].presented at the 2011 SEG Annual Meeting,2011.

[22] Zhang H,et al.Joint geophysical imaging of the Utah area using seismic body waves, surface waves and gravity data:Eos Trans[J].presented at the AGU Fall Meeting Abstracts,2009.

[23] Yang Y J,Ritzwoller M H,Jones C H.Crustal structure determined from ambient noise tomography near the magmatic centers of the Coso region,southeastern California[J].Geochemistry,Geophysics,Geosystems,2011,12 (2).

[24] Vlahovic G,Elkibbi M,Rial J A.Shear-wave splitting and reservoir crack characterization:the Coso geothermal field[J].J Volcanol Geoth Res,2003,120(1):123-140.

[25] Lou M,Shalev E,Malin P E.Shear-wave splitting from micro-earthquakes seismograms in the Northwest Geysers,California[J].EOS,1997,77(46):513.

[26] Rial J A,Elkibbi M,Yang M.Shear-wave splitting as a tool for the characterization of geothermal fractured reservoirs:lessons learned[J].Geothermics,2005,34:365-385.

[27] Elkibbi M, Rial J A.The Geysers geothermal field:results from shear-wave splitting analysis in a fractured reservoir[J].Geophys J Int,2005,162:1024-1035.

[28] Verdon J P,Kendall J M.Detection of multiple fracture sets using observations of shear-wave splitting in microseismic data[J].Geophysical Prospecting, 2011,59:593-608.

[29] Simiyu S M,Malin P E.A "Volcanoseismic" approach to geothermal exploration and reservoir monitoring:Olkaria,Kenya and Casa Diablo//Kyushu-Tohoku:The Proceedings of the World Geothermal Congress 2000,2000.

[30] Hough S E,Lees J M,Monastero F.Attenuation and source properties at the Coso Geothermal Area,California[J].B Seismol Soc Am,1999,89(6):1606-1619.

[31] Muksin U,Haberland C,Bauer K,et al.Three-dimensional upper crustal structure of the geothermal system in Tarutung (North Sumatra, Indonesia) revealed by seismic attenuation tomography[J].Geophysical Journal International,2013,195:2037-2049.

[32] Wu H T,Lees J M.Attenuation structure of Coso geothermal area,California,from wave pulse widths[J].B Seismol Soc Am, 1996,86 (5):1574-1590.

[33] Sanders C,Ho-Liu P,Rinn D,et al.Anomalous shear wave attenuation in the shallow crust beneath the Coso volcanic region,California[J].Journal of Geophysical Research:Solid Earth(1978–2012),1988,93(B4):3321-3338.

[34] Wei S J,DeAngelo M V,Hardage B A.Advantages of joint interpretation of P-P and P-SV seismic data in geothermal exploration[J].Interpretation,2014,2(2):117-123.

[35] Wang J,Sun Z.Amazing geothermal[M].Beijing:Tsinghua University Press,2001.

[36] Casini M,Ciuffia S,Fiordelisi A,et al.Results of a 3D seismic survey at the Travale (Italy) test site[J].Geothermics,2010,39(1):4-12.

[37] Wei S J,DeAngelo M V,Hardage B A.Interpretation of multicomponent seismic data across Wister geothermal field,Imperial Valley,California[J].Interpretation,2014,2(2):125-135.

[1] 陈秀娟, 刘之的, 刘宇羲, 柴慧强, 王勇. 致密储层孔隙结构研究综述[J]. 物探与化探, 2022, 46(1): 22-31.
[2] 石磊, 管耀, 冯进, 高慧, 邱欣卫, 阙晓铭. 基于多级次流动单元的砂砾岩储层分类渗透率评价方法——以陆丰油田古近系文昌组W53油藏为例[J]. 物探与化探, 2022, 46(1): 78-86.
[3] 张建智, 胡富杭, 刘海啸, 邢国章. 煤矿老窑采空区地—井TEM响应特征[J]. 物探与化探, 2022, 46(1): 191-197.
[4] 刘仕友, 张明林, 宋维琪. 基于曲波稀疏变换的拉伸校正方法[J]. 物探与化探, 2022, 46(1): 114-122.
[5] 王迪, 张益明, 牛聪, 黄饶, 韩利. 压制孔隙影响的流体敏感因子优选及其在烃类检测中的应用[J]. 物探与化探, 2021, 45(6): 1402-1408.
[6] 芮拥军, 尚新民. 胜利油田非一致性时移地震关键技术探索与实践[J]. 物探与化探, 2021, 45(6): 1439-1447.
[7] 王飞, 孙亚杰, 裴金梅, 宋建国, 李文建. 高密度单点接收地震采集数据的处理方法讨论[J]. 物探与化探, 2021, 45(6): 1469-1474.
[8] 刘兰锋, 尹龙, 黄捍东, 周振亚, 董金超. 一种基于岩石物理建模的横波预测方法[J]. 物探与化探, 2021, 45(6): 1482-1487.
[9] 徐浩, 吴小平, 盛勇, 廖圣柱, 贾慧涛, 徐子桥. 微动勘探技术在城市地面沉降检测中的应用研究[J]. 物探与化探, 2021, 45(6): 1512-1519.
[10] 张豪, 辛勇光, 田瀚. 基于双相介质理论预测川西北地区雷口坡组储层含气性[J]. 物探与化探, 2021, 45(6): 1386-1393.
[11] 韦红, 白清云, 张鹏志, 甄宗玉. 基于反褶积广义S变换的双相介质理论油水识别法在渤海S油田馆陶组的应用[J]. 物探与化探, 2021, 45(6): 1394-1401.
[12] 魏岩岩, 吴磊, 周道卿, 肖安成, 黄凯. 柴达木盆地西部阿拉尔断裂新生代构造变形特征及意义[J]. 物探与化探, 2021, 45(5): 1171-1178.
[13] 张振宇, 袁桂琴, 孙跃, 王之峰. 地质调查地球物理技术标准现状与发展趋势[J]. 物探与化探, 2021, 45(5): 1226-1230.
[14] 朱颜, 韩向义, 岳欣欣, 杨春峰, 常文鑫, 邢丽娟, 廖晶. 致密砂岩储层脆性测井评价方法研究及应用——以鄂尔多斯盆地渭北油田为例[J]. 物探与化探, 2021, 45(5): 1239-1247.
[15] 雍凡, 刘子龙, 蒋正中, 罗水余, 刘建生. 城市三维地震资料处理浅层成像关键技术[J]. 物探与化探, 2021, 45(5): 1266-1274.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
京ICP备05055290号-3
版权所有 © 2021《物探与化探》编辑部
通讯地址:北京市学院路29号航遥中心 邮编:100083
电话:010-62060192;62060193 E-mail:whtbjb@sina.com