摘要
我国有近300×104 km2的蓝色国土,其中蕴藏着丰富的油气资源。然而,我国对海洋中油气资源的勘探、开发起步较晚,各个海域的油气资源的勘探程度较低,对油气资源的探明程度就更低。各海域中南黄海盆地尤为特殊,是我国目前惟一未发现油气田(藏)的海域。据学者们研究,南黄海盆地处于扬子地块之上,志留系上统和泥盆系下统缺失,中生代和古生代海相碳酸盐岩地层发育较完整,地层发育相对厚、分布区域广,具有较好的含油气勘探前景。然而,由于南黄海盆地勘探程度低,受种种因素的制约,对该海域的地质认识还不够清晰。由于该海域的特殊自然环境和地质现象导致野外采集资料有其特殊性,各种噪音发育、深部反射能量弱、特别严重的是该海域地震资料的各种多次波种类繁多、能量强且多次波的波场特征十分复杂,给后续高质量的室内资料处理带来诸多困难,开展进一步的解释研究工作就更加不易。为此,改善该海域地震资料的品质迫在眉睫,不但要保证野外施工质量,更要在处理中下功夫,尽可能的获得高质量的处理剖面。在该海域地震资料处理中在做好噪音压制的同时,最重要的是要摸清该海域地震资料复杂多次波形成机理、并研究合理有效的多次波压制技术,有的放矢,去伪存真,得好真实可靠的地震剖面,为后续解释研究工作的顺利开展打下坚实的基础。
近几年,配合南黄海海域野外采集技术攻关研究,开展了大量的室内处理技术研究以改善地震资料的处理品质,开展了随机噪音压制技术研究、相干噪音压制技术研究和多次波压制技术研究,特别是就严重制约该海域地震资料处理质量的复杂多次波压制技术开展了大量研究工作。该论文重点研究南黄海海域复杂多次波的形成机理及相应的多次波压制技术。本学位论文依托于国家专项之《南黄海综合地球物理补充调查》和国家“863”计划(2006AA09Z339)研究完成的。
该论文研究取得了如下几项创新性成果：
1.基本摸清了南黄海海域地震资料复杂多次波的形成机理
利用搜集的测井资料和他人的研究成果,建立地质模型,采用声波方程和弹性波波动方程正演模拟,作者对比分析了模拟记录的波场特征,特别是多次波的特征,结合实际资料开展综合分析研究,基本摸清了该海域地震资料虚反射、鸣震、强反射界面反射多次波、折射多次波及层间多次波等各种复杂多次波的形成机理,为研究该海域合理的多次波压制技术提供支撑。
2.首次采用曲波变换技术有效压制南黄海海域地震资料折射多次波和转换多次波
该海域存在T2等多套强反射层的特殊地质现象,入射角极易达到临界角,产生强折射波,进而形成折射多次波,加之采集排列大,入射角范围广,及地下介质的复杂多样,产生复杂的转换波及转换多次波,研究利用E.J.Candes等提出的曲波变换技术有效压制南黄海海域地震资料的折射多次波和转换多次波。
3.在南黄海海域地震资料强多次波压制处理中首次采用高精度τ-R变换技术取得显著效果
该海域地震资料多次波种类繁多,如虚反射、鸣震、海底及强反射界面全程多次波和层间多次波、转换多次波以及折射多次波发育,波场特征复杂,通过正演模拟分析和实际资料研究,对这些多次波的形成机理有了清晰认识,进而开展有效的多次波压制技术研究。针对该海域强反射界面多次波和层间多次波十分发育的特殊性,综合分析当今国内外各种多次波压制技术优缺点,及这些技术对压制该海域多次波的局限性,首次采用李庆忠院士提出的高精度τ-R变换技术压制多次波,通过对理论模拟记录和实际资料的处理,对强反射界面多次波和层间多次波的压制取得较好的效果,特别对层间多次波的压制有其独到之处。
4.形成一套合理压制南黄海海域地震资料复杂多次波的技术方案
针对该海域地震资料多次波种类繁多,波场特征复杂的特殊性。综合研究,形成一套合理压制南黄海海域地震资料复杂多次波的技术方案：在合理压制各种噪音的基础上,首先采用自由表面多次波压制技术(SRME)衰减自由表面多次波、接着采用曲波变换技术压制折射多次波和转换多次波、然后结合组合反褶积进一步压制鸣震、继而用高精度τ-R变换技术压制强反射界面全程及层间多次波,在各种多次波得到基本压制后,速度分析精度提高,再在动校正之后采用剔除拟合叠加技术代替常规的叠加技术,将残余多次波进一步压制,获得高质量的处理剖面。
以上多项处理技术的研究完善及有机融合,形成一套合理压制南黄海海域地震资料复杂多次波的技术体系和方案,能够很好的压制该海域的复杂多次波。在合理压制掉多次波后,为获得高品质的地震剖面提供保障,为后续研究认识南黄海海域地质特征打下坚实基础。
China has nearly 300x104km2 blue lands, which is rich in oil and gas resources. However, the exploration and development of China's oil and gas resources in the ocean started late. The exploration degree of oil and gas resources in all waters is lower and the proven degree of oil and gas resources is much lower. The South Yellow Sea Basin is particularly special, which is the only sea area without oil and gas (reservoir) in China at present. According to scholars'study, the South Yellow Sea Basin is above the Yangtze block, where the upper Silurian and lower Devonian is missing, and Mesozoic and Paleozoic marine carbonate rocks develop completely. The stratigraphic development is relatively thick, and the distribution of area is wide, which has good oil and gas exploration prospects. However, due to the low level of exploration of the South Yellow Sea Basin, affected by various factors, the geological knowledge of the waters is also not clear enough. The acquired seismic data has its own particularity because of the special natural environment and geological phenomena of the area. There is all kinds of noise and deep reflection energy is weak, which is especially serious is that there are various multiple-waves that have high energy and complex wave field characteristics on seismic data of the area. It brings many difficulties to the high-quality indoor data processing and to carry out further interpretation research work is even more difficult. So it is imminent to improve the quality of seismic data of the area, which is not only to ensure the wild construction quality, but also to improve the process method to acquire high-quality processing profile. When suppressing noise in seismic data processing of the area, the most important problem is to find out that the mechanism of the complex multiple-waves on seismic data of the area, and to consider reasonable and effective multiple suppression techniques. Eliminate the false and retain the true to get well real and reliable seismic profiles and lay a solid foundation for the following interpretation work.
In recent years, with the South Yellow Sea field acquisition technology research study, we carried out a large number of indoor processing technology research to improve the processing quality of seismic data and carried out technical studies to suppress random noise, coherent noise suppression technology research and multiple suppression technology research, especially doing a lot of research on complex multiple suppression technologies which severely constrained the seismic data processing quality of the waters. The paper focuses on the South Yellow Sea complex multiple wave formation mechanism and the corresponding multiple-wave suppression technology. This dissertation relies on the National project, "Integrated geophysical supplementary investigations in Southern Yellow Sea" and the National "863" program (2006AA09Z339) study.
The thesis has made a number of innovative achievements as follows:
1. Basically found out the formation mechanism of complex multiple wave on seismic data of South Yellow Sea.
Establish a geological model by using of log data collected and other people's research results. The author analyze comparatively wave field characteristics of analog records, especially the multiple wave characteristics by using acoustic wave equation and the elastic wave equation forward modeling. By developing an integrated analysis with practical seismic data, basically find out the formation mechanism of virtual reflection, reverberation, reflection multiple wave on strong reflection interface, refraction multiple, interbed multiple and other complex multiple wave on the seismic data of this area, which provides support for the study of the reasonable multiple-wave suppression technology of the area.
2. Curvelet transform technology was used to effectively suppress the refraction multiple wave and converted multiple wave on seismic data of South Yellow Sea for the first time.
The existence of special geological phenomenon of many sets of strong reflective layers such as T2 of the sea making the incident angle easily achieve the critical angle, resulted in strong refraction and formed refraction multiple-wave. At the same time, converted wave and converted multiple-wave of the sea developed because the collection array was large, the large range of the incident angle and the complexity of the underground media, effectively suppress the refracted multiple wave and converted multiple-wave by using Curvelet Transform Technology proposed by E.J.Candes on the South Yellow Sea seismic data.
3. The high-precisionτ-R Transform technology was firstly used to effectively suppress strong multiple waves of the South Yellow Sea seismic data.
There are various multiple-waves on the South Yellow Sea seismic data, such as the virtual reflection, reverberation, the whole multiple waves of submarine and strong reflective interface, interbed multiple waves, converted waves and refracted multiple waves. The wave field characteristics are complex. There is a clear understanding of the formation mechanism of these multiple waves through the forward modeling analysis and the studies of practical data, and thus to carry out research on effective multiple-wave suppression technology. Against the special nature of the development of strong reflection multiple and interbed multiple, by the comprehensive analysis of advantages and disadvantages of current multiple suppression technology at home and abroad and the limitations of these technologies on repression of multiple waves of the waters, we proposed to suppress multiple reflections by using high-precisionτ-R transformation technology proposed by Li Qingzhong Fellow. Through the processing of theoretical analog records and the actual data, there was a good result on the repression of multiple waves of strong reflecting interface and interbed multiple waves. It has its own unique especially for the repression of interbed multiple waves.
4. Form a reasonable technical program to suppress the complex multiple wave of the South Yellow Sea seismic data.
Against the particularity that there are various multiple waves the complex wave field characteristics on seismic data of the sea. Through comprehensive study, we formed a reasonable technical solution to suppress the complex multiple wave of the South Yellow Sea seismic data:on the basic of the reasonable suppression of a variety of noise, first use the free surface multiple suppression techniques (SRME) with deconvolution to attenuate the free surface multiple reflections, and then use curvelet transform technique to suppress refracted multiple wave and converted multiple waves, followed by using high-precisionτ-R transform technique to suppress whole and interbed multiple reflections on strong reflection interface. After a variety of multiples to be suppressed, the velocity analysis precision was improved, and then use deletion fitting stacking technique to replace conventional stacking technique after normal moveout correction to further suppress the residual multiple reflections and to acquire high-quality processing profile.
The improvement of many kinds of processing technology above and the formation of a reasonable technology system and program to suppress the complex multiple wave of South Yellow Sea seismic data can effectively suppress the multiple reflections in the waters. After reasonably suppressing the multiple reflections, provide protection for obtaining high-quality seismic profiles and lay a solid foundation for the follow-up study of the geological features of the South Yellow Sea.
引文
[1]邱中建,方辉.对我国油气资源可持续发展的一些看法.石油学报,2005,26(3)：1-5
[2]潘继平,张大伟,岳来群,等.全球海洋油气勘探开发状况与发展趋势.中国矿业,2006,15(11)：1-4
[3]李种,张猛,刘百芳,等.论我国石油供给发展战略.福建论坛·人文社会科学版,2009,6：9-14
[4]彭韩铭.从“东海之争”看中国大国之略.法制与会,2009,6(下)：186-187
[5]吕晓伟.南海争端的现状、原因及对策.当代社科视野,2009,7-8：75-80
[6]马立桥,董庸,屠小龙,等.中国南方海相油气勘探前景.石油学报,2007,28(3)：1-7
[7]范小林.南黄海盆地海相领域油气勘探战略思考.海相油气地质,2001,6(4)：35-40
[8]戴春山,杨艳秋,闫桂京.南黄海中-古生代海相残留盆地埋藏生烃史模拟及其意义.石油与天然气地质,2005,26(1)：49-56
[9]龚建民,陈建文,何拥军,等.低层大气烃类检测预测南黄海盆地油气远景.海洋地质与第四纪地质,2006,2(7)：75-79
[10]肖国林.南黄海盆地油气地质特征及其资源潜力再认识.海洋地质与第四纪地质,2002,22(2)：81-87
[11]郝天珧,SUN Mancheol,王谦身,等.根据重力数据研究黄海周边断裂带在海区的延伸.地球物理学报,2002,45(3)：385-397
[12]王谦身,安玉林.南黄海西部及邻域重力场与深部构造.科学通报,1999,44(22)：2448-2451
[13]冯志强,姚永坚,曾祥辉,等.对黄海中、古生界地质构造特征及油气远景的新认识.中国海上油气(地质),2002,16(6)：365-373
[14]李刚,陈建文,肖国林,等.南黄海海域的海相中—古生界油气远景.海洋地质动态,2003,19(8)：12-16
[15]陈建文,肖国林,刘守全,等.中国海域油气资源勘查战略研究.海洋地质与第四纪地质,2003,23(4)：77-82
[16]吴志强.黄海地层岩石地球物理特征及其对地震勘探技术的挑战.中国海上油气(地质),2003,17(6)：407-411
[17]吴志强.南黄海中部隆起海相地层油气地震勘探关键技术研究：[博士学位论文].青岛：中国海洋大学,2009
[18]莫杰.我国海上油气勘探开发展现好前景.海洋地质动态,1997,2：20-22
[19]陈建文.南黄海盆地油气勘探战略选区.海洋地质动态,2002,18(11)：28-29
[20]李鹏,刘伊克,常旭,等.多次波问题的研究进展.地球物理学进展,2006,21(3)：888-897
[21]Verschuur D J,Berkhout A J,Wapenaar C P A. Adaptive surface-related multiple elimination. Geophysics,1992,57(9),1166-1177
[22]Berkhout A J,Verschuur D J. Estimation of multiple scattering by iterative inversion,Part LTheoretical considerations. Geophysics,1997,62 (5),1586-1595
[23]Monk D J. Waveequation multiple suppression using constrained gross-equalization Geoghysics Prospecting,1993,41,725-736
Wang Y. Multiple subtraction using an expanded multichannel matching filter. Geophysics, 68,346-354
[25]Uma Shankar,ORIGINAL RESEARCH.Signal enhancement and multiple suppression using Radon transform:an application to marine multichannel seismic data. Mar Geophys Res 2009 (30):85-93
[26]Shashank,Shekhar,SinghKalachand Sain..Multiple attenuation in complex geology with a pattern-based approach Antoine Guitton. GEOPHYSICS2005,VOL.70,NO.4
[27]Anh Kiet Nguyen and Matthias Riede. Fast free surface multiples attenuation workflow for three-dimensional ocean bottom seismic data barbel Traub. Geophysical Prospecting,2009,57,785-802
[28]CBucy filter Marcus P.C. Rocha, Lourenildo W.B. Leite, Mauro de L. Santos Valcir J.da C. Farias.Attenuation of multiple in reflection seismic data using Kalman.AppliedMathematics ,2007,805-815
[29]邢涛,张训华,张维冈.南黄海地球物理调查研究现状.海洋地质动态,2005,21(6)1-4
[30]王连进,叶加仁,吴冲龙.南黄海盆地前第三系油气地质特征.天然气工业,2008,25(7)：1-3
[31]王志,贺振华,薛彬,等.广角反射研究及高斯射线正演模拟分析.成都理工学院学报,2002,29(1)：9-16
[32]杨贵祥,贺振华,朱兹.中国南方海相地层下组合地震采集方法研究.石油物探,2006,3,(2)：157-168
[33]吴律.τ-P变换及应用.北京：石油工业出版社,1993
[34]牛滨华,沈操,黄新武,等.波动方程多次波压制技术的进展.地球物理学进展,2002,17(3)：480-485
[35]王维红,首皓,刘洪等.线性同相轴波场分离的高分辨率：τ-P变换法.地球物理学进展.2006,21(1)：74-78
[36]王维红,刘洪.道均衡抛物线Radon变换法地震道重建.石油地球物理勘探.2005,40(5)：518-522
[37]黄新武,吴律,牛滨华.基于抛物线拉东变换的地震道重构.中国矿业大学学报.2003,32(5)：534-539
[38]王维红,崔宝文.双曲Radon变换法多次波衰减.新疆石油地质,2007,28(3)：363-365
[39]王维红,陈树民,王建民.预测切除抛物Radon变换表面多次波衰减方法CPS/SEG Beijing 2009, Expanded Abstracts. ID 1122
[40]罗小佳,朱仕军,刘二军,等.最优化相似加权Radon变换压制多次波.勘探地球物理进展,2009,32(3)：186-188
[41]郑旭刚,张军华,等Curvelet变换及其在地震资料去噪中的应用.中国地球物理会,2008：465
[42]刘冰,王德利Curvelet软阈值迭代去噪法.中国地球物理会,2008：396
[43]张恒磊,张云翠,等.基于Curvelet域的叠前地震资料去噪方法.石油地球物理勘探,2008,43(5)：508-515
[44]彭才,常智,等.基于曲波变换的地震数据去噪方法.石油物探,2008,47(5)：561-565
[45]耿瑜,吴帮玉,等.地震数据的Curvelet压缩方法.中国地球物理会,2007：579
[46]包乾宗,高静怀,等Curvelet域垂直地震剖面波场分离.西安交通大学学报,2007,41(6)：155-159
[47]张建贵Hyp-Curvelet变换与多次波的识别、分离和压制：[博士学位论文].长沙：中南大学,2002
[48]张素芳,徐义贤,等.基于Curvelet变换的多次波去除技术.石油地球物理勘探,2006,41(3)：262-267
[49]White R E. A multichannel method of multiple attenuation based on hyperbolic moveout curves. 50th EAEG Meeting, the Hague, Extended Abstracts:1988,1-22
[50]胡天跃,王润秋,WhiteR地震资料处理中的聚束滤波方法.地球物理学报.2000,43(1)：105-115
[51]洪菲,胡天跃,王润秋.利用三维聚束滤波方法消除相关嗓声.石油地球物理勘探,2005,40(1)：42-47
[52]张金强,牟永光.多次波压制的自适应方法.石油地球物理勘探,2002,37(3)：209-215
[53]牛滨华,沈操,黄新武,等.波动方程压制多次波的技术方法.地学前缘,2002,(02)：11-14
[54]丁科,宋守根,谢忠球.逆散射理论的发展及应用前景.地球物理学进展,2005(03)：22-27
[55]范承亮,丁科,张建贵,等.逆散射成像的算法.中南工业大学学报(自然科学版),2001(04)：15-21
[56]谭绍泉, 徐淑合,朱卫强,等.基于波动理论消除表层多次波.石油大学学报(自然科学版)2004(05)：25-33
[57]崔树果.东海海域自由表面多次波压制方法研究：[博士学位论文].青岛：中国海洋大学,2008
[58]姜玉坤.南黄海盆地地震资料处理方法初探.海洋地质动态,2002,18(11)：36-38
[59]张一波.南黄海多次波特征及压制方法研究：[硕士学位论文].青岛：中国海洋大学,2009
[60]张一波,刘怀山,吴志强.南黄海多次波特征及其速度分析.海洋地质动态,2008,24(8)：8-13
[61]吴志强,陆凯,闫桂京,陈建文.南黄海前新生代油气地球物理勘探方法.海洋地质动态,2008,4(8)：1-7
[62]冯永强,石平,薛爱民,等.南黄海前新生代地震资料处理实践.海洋地质动态,2008,24(8)：26-32
[63]李庆忠.用剔除拟合法求纵波正入射剖面—一种取代水平叠加的处理技术.石油地球物理勘探,1995,130(2)：147-167
[64]万欢.高保真多次波剔除法及其在海上地震资料处理中的应用.中国海上油气,2005,117(2)：163-166
[65]姚永坚,夏斌,冯志强,等.南黄海古生代以来构造演化.石油实验地质,2005(02)：15-18
[66]蔡乾忠.中国东部与朝鲜大地构造单元对应划分.海洋地质与第四纪地质,1995,15(1)：7-19
[67]索书田,钟增球,游振东.大别—苏鲁造山带中朝与扬子克拉通三叠纪碰撞缝合带位置究竟在何处?.地质科技情报,1999,18：2
[68]王清晨,从柏林,朱日祥.大别山超高压变质岩带形成的地球动力学.寸丹集-庆贺刘光鼎院士工作50周年学术论文集,1998
[69]秦蕴珊, 赵一阳,等.黄海地质(黄海海底与地壳结构).青岛：海洋出版社,1989
[70]张金川.南黄海海域构造单元的重新命名及其特征对比.海洋地质动态,1995,06：3-5
[71]戴明刚.黄海地质与地球物理特征研究.地球物理学进展,2003,4(8)：583-591
[72]陈沪生.扬子准地台下扬子盆地HQ-13线地球物理-地质综合解释纲要.中国南方油气勘探新领域探索论文集(2),1988：239-249
[73]邓红婴.中下扬子区震旦纪—中三叠世海相盆地类型及后期改造.海相油气地质,1999,4(3)：38-45
[74]郑求根,蔡立国,丁文龙,等.黄海海域盆地的形成与演化.石油与天然气地质,2005,26(5),647-654
[75]冯志强,陈春峰,姚永坚,等.南黄海北部前陆盆地的构造演化与油气突破.地学前沿,2008,15(6)：219-231
[76]王潦亮,易海,姚永坚,等.南黄海海域晚古生代一新生代沉积演化特征.南海地质研究,2002,00：15-28
[77]王金渝,周荔青,郭念发,等.苏浙皖石油天然气地质.北京：石油工业出版社,2000
[78]朱光,徐嘉炜,刘国生,等.下扬子地区前陆变形构造格局及其动力学机制.中国区域地质,1999,18(1)：74-79
[79]闫吉柱,俞凯,赵曙白,等.下扬子区中生代前陆盆地.石油实验地质,1999,21(2)：95-99
[80]陈沪生.下扬子地区重建型海相烃源油气领域评价及勘探对策.海相油气地质,2002,6(7)：33-41
[81]李刚,陈建文,肖国林,等.黄海海域陆相中生界油气远景.海洋地质动态,2003,19(8)：7-11
[80]陈建文,吴志强.南黄海盆地油气地质研究进展.海洋地质动态,2002,18(1)：22
[81]李刚,吴时国.南黄海海域的海相地层含油气系统.海洋地质动态,2007,23(7)：27-32
[82]李刚,张燕,陈建文,等.黄海海域陆相中生界地震反射特征及靶区优选.中国海洋大学学报,2004,34(6)：1069-1074
[85]张家强.南黄海中、古生界油气勘探前景.海洋地质动态,2002,18(11)：25-27
[86]龚建明,陈建文,何拥军,等.低层大气烃类检测预测南黄海盆地油气远景.海洋地质与第四纪地质,2006,26(1)：75-79
[87]陆基孟.地震勘探原理.东营：中国石油大学出版社,2009
[88]韩世春.各向异性介质转换波速度分析方法研究及应用：[硕士学位论文].东营：中国石油大学,2007
[89]董良国,李国治,杨全荣,等.横向各向同性介质中弹性波的物理模拟.石油物探,1999,38(1)：76-85
[90]李晓光,多波多分量数值模拟与数据处理方法：[硕士学位论文].北京：中国地质大学,2006
[91]K.Sen.Numerical modeling of wave equation by a truncated high-order finite-difference method.Earthquake Science.Earthq Sci (2009) 22:205-213
[91]彭菲.人工源和随机源激发地震波的时域有限差分模拟研究：[硕士学位论文].北京：中国地震局预测研究所,2008
[93]陈宇红.二维电磁场的有限元计算：[硕士学位论文].大连：大连理工大学,2001
[94]范学平,黄建民,吴宏.边界元法用于油气藏稳定渗流数值模拟研究.天然气工业,1996,12(16)：30-33
[95]王元淳.边界元法基础.上海：上海交通大学出版社,1989
[96]黄天俊.EDA介质地展波场数值模拟研究：[硕士学位论文].成都：成都理工大学,2005
[97]Berkhout, A. J.. Applied seismic wave theory. Elsevier Science Publ. co.,Inc.,1987
[98]Virieux J.SH-wave propagation in heterogeneous media:velocity-stress finite-difference method. Geophysics,1984,49(11):1933-1957
[99]董良国,马在田,曹忠景,等.一阶弹性波方程交错网格高阶差分解法.地球物理学报,2000,3(43)：411-419
[100]曾有良Radon变换波场分离技术研究：[硕士学位论文].东营：中国石油大学,2007
[101]肖姹莉,赵世昌：τ-p变换中几个问题的探讨.石油物探,1985,24(2)：29-45
[102]顾建平.改进的Radon滤波压制多次波技术及应用效果.石油地球物理勘探,2003,11(38)：38-41
[103]黄新武,吴律,牛滨华,等.抛物线Radon变换中的参数采样与假频.石油大学学报(自然科学版),2003,27(2)：27-31
[104]张军华,吕宁,雷凌,等.抛物线拉冬变换消除多次波的应用要素分析.石油大学学报(自然科学版),2004,39(4),388-393
[105]朱生旺,魏修成,李锋.用抛物线Radon变换稀疏解分离和压制多次波.石油地球物理勘探,2002,37(2)：110-115
[106]刘喜武,刘洪,李幼铭.高分辨率Radon变换方法及其在地震信号处理中的应用.地球物理学进展,2004,1(19)：008-015
[107]White R E. A multichannel method of multiple attenuation based on hyperbolic moveout curves.50th EAEG Meetingthe Hague, Extended Abstracts:1988,1-22
[108]胡天跃,王润秋,WhiteR地震资料处理中的聚束滤波方法.地球物理学报,2000,43(1)：105-115
[109]Hong F, Wang R. Target multiple attenuation using 3D beamforming. The 73th SEG Annual Meeting,ExpandedAbstracts:2003.1969-1972
[110]Shumway R H, Dean W C. Best linear unbiased estimation for multivariate stationary processes. Technometrics,1968,10 (3):523-534
[111]Frost O L. An algorithm for linearly constrained adaptive array processing .Proceedings of theIEEE,1972,60 (8):926-935
[112]Hykin S.Adaptive Filter Theory (4th edition).NJ:Prentice Hall,2002
[113]胡天跃,王润秋,温书亮.聚束滤波方法消除海上地震资料的多次波.石油地球物理勘探,2002,37(1)：18-23
[114]王润秋,胡天跃.用聚束滤波方法消除地震资料中规则噪音.勘探地球物理进展,2003,26(4)：268-272
[115]洪菲,胡天跃,张文坡,等.用优化聚束滤波方法消除低信噪比地震资料中的多次波,地球物理学报,2004,47(6)：1106-1110
[116]Berkhout A J. Seismic Migration:Imaging of acoustic energy by wave field extrapolation.Elsevier Scientific Pub.Com.,1982
[117]Verschuur D J,Berkhout A J,Wapenaar C P A.Wavelet estimation by prestack multiple elimination.59th Ann.Internat.Mtg.,Soc.ExplGeophys,Expanded abstracts,1994:1129-1132
[118]Wapenaar C P A,Herrmann P,Verschuur D J,Berkhout A J. Decomposition of multi-component seismic data into primary P-and S-wave responses. Geophys.Prosp.,1990,38 :634-81
[119]Verschuur D J,Berkhout A J,Wapenaar C P A.Adaptive surface-related mutiple elimination.Geophysics,1992,57 (9):1166-1177
[120]Dragoset, B., and MacKay, S.. Surface multiple attenuation and subsalt imaging in 63rd Ann. Internat. Mtg. Soc. of Expl. Geophys.,1993:1099-1102
[121]Berkhout A J,Verschuur D J.Estimation of multiple scattering by iterative inversion,Part I: Theoretical considerations. Geophysics,1997,62 (5):1586-1595
[122]Verschuur D J,Berkhout A J.Estimation of multiple scattering by iterative inversion,PartII: Practical aspects and examples. Geophysics,1997,62 (5):1596-1611
[123]沈操.基于波动方程的自由界面多次波压制：[博士学位论文].北京：中国地质大学,2003
[124]Berkhout A J.Multiple removal based on the feedback model[J].The Leading Edge,1999,18 (1):127-131
[125]Kelamis P G, Verschuur D J. Surface-related multiple elimination on land seismic data-Strategies via case studies. Geophysics,2000,65 (3):719-734
[126]Dragoset, W. H., and Jericevic, Z.. Some remarks on surface multiple attenuation:Geophysics, 1998,63:772-789
[127]Wang, Y., and Levin, S. A.. An investigation into eliminating surface multiples. SEP.1994, 80:589-602
[128]Hugonnet, P.. Partial surface related multiple elimination in 72nd Ann. Internat. Mtg. Soc. of Expl. Geophys.,2002,2104-3005
[129]E. J. Candes, and D. L. Donoho, "Curvelets-A surprisingly effective nonadaptive representation for objects with edges," Technical Report, Larry L. Schumaker, Eds. Nashville: Vanderbilt University Press,1999, pp.1-10
[130]E. J. Candes, and F. Guo, "New multiscale transforms, minimum total variation synthesis: Applications to edge-preserving image reconstruction," Signal Processing, vol.82, pp.1519-1543, 2002
[131]E. J. Candes, and D. L. Donoho, "New tight frames of curvelets and optimal representations of objects with piecewise C2 singularities," Communications on Pure and Applied Mathematics, vol.57, pp.219-266,2004
[132]E. J. Candes and L. Demanet, "The curvelet representation of wave propagators is optimally sparse," Communications on Pure and Applied Mathematics, vol.58, pp.1472-1528,2005
[133]J. L. Starck, E. J. Candes and D. L. Donoho, "The Curvelet Transform for Image Denoising," IEEE Transactions on Image Processing, vol.11, pp.670-684,2000
[134]Linfei Wang, Huaishan Liu, Siyou Tong,Jing Zhang,Zhiqiang Wu. Curvelet-based noise attenuation in prestack seismic data. IEEE Computer Society, Proceedings of ETT and GRS 2008,Shanghai.Vol.2,61-64. (EI:,ISTP)
[135]宋英姿.第二代Curvelet变换及其在图像融合中的应用：[硕士学位论文].南京：河海大学,2007
[136]G. Hennenfent and F. J. Herrmann, "Seismic denoising with non-uniformly sampled curvelets," IEEE Computing in Science and Engineering, vol.8, pp.16-25,2006
[137]F. J. Herrmann, "Optimal imaging with curvelets," SEG Expanded Abstracts, vol.22, pp. 997-1000,2003
[138]Felix J. Herrmann, Deli Wang, Gilles Hennenfent, and Peyman P. Moghaddam.2008, Curvelet-based seismic data processing:A multiscale and nonlinear approach. Geophysics,Vol.73, NO.P.A1-A5
[138]Candes,E.J.,L.Demanet,D.L.Donoho,andL.Ying,2006a,Fastdiscrete curvelet transforms:SIAM Multiscale Modeling and Simulation,5,861-899
[140]仝中飞Curvelet阈值迭代法在地震数据去噪和插值中的应用研究：[硕士学位论文].长春：吉林大学,2009
[141]李庆忠.走向精确地震勘探的道路.北京：石油工业出版社,1995
[142]Tong Siyou, Wang Linfei, Liu Huaishan, Zhang Jin, Wang Ruimin. Marine linear noise suppression in the curvelet domain. IEEE Computer Society, Proceedings of IFITA 2009, Chengdu,China. Vol.2,186-189
[143]张雅勤,张关华,宁俊瑞.海上船噪声干扰的压制技术.物探与化探,2001,25(4)290-293
[144]姚伯初,王衍棠,伍忠良,等.南黄海盆地的地震方法试验.南海地质研究,2002,129-23
[145]胡天跃.地震资料叠前去噪技术的现状与未来.地球物理学进展,2002,17(2)：219
[146]熊翥.复杂地区地震数据处理思路.北京：石油工业出版社,2002
[147]董敏煜.地震勘探.东营：石油大学出版社,2004
[148]Duncan,G..Beresford, G.. Slowness adaptive f-k filtering of prestack seismic data. Geophysics,1994,59(1)140-147
[149]童思友,徐磊磊,崔树果,刘怀山.南黄海地震资料叠前有源干扰的自动识别与压制.海洋地质动态,2008,24(8)：14-19