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压裂诱发的微地震震源机制及信号传播特性

Keywords: 微地震,破裂机制,震源机制解,矩张量,裂隙演化

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Abstract:

?随着仪器、处理和解释技术的进步,微地震在描绘储层内的压裂和断裂系统方面的应用愈来愈广,在储层管理上发挥了越来越大的作用.本文分析了压裂产生的脆性变形以及微地震产生机制,探讨了裂隙动态变化及产生的微地震响应特性,分析了利用微地震数据研究裂隙时空分布规律的可能性.主要内容包括:裂纹的产生诱发微地震,在水力压裂过程中裂纹尖端效应和漏泄效应是产生微地震的主要原因;微地震震源矩张量釆用特征值分解法可以分解为双力偶成分、补偿线性矢量极偶成分和各向同性成分;通过有限差分正演模拟分析了微地震信号的传播特性,微地震源特性和速度模型会显著影响微地震波形.

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[4]  mengzhaobo,yanglihua.numericalsimulationofsourcemechanisminseismicprospecting[j].ogp.1990,25(1):45-52??浏览
[5]  janskyj.plickavandeisnerl.feasibilityofjoint1dvelocitymodelandeventlocationinversionbytheneighbourhoodalgorithm.geophysicalprospecting,2010,58(2):229-234.
[6]  angusda.aone-waywaveequationformodelingseismicwaveformvariationsduetoelasticheterogeneity[j].geophysicaljournalinternational.2005,162(3):882-898
[7]  angusda,kendalljm,fisherqjetal.modellingmicroseismicityofaproducingreservoirfromcoupledfluid-flowandgeomechanicalsimulation[j].geophysicalprospecting.2010,58(5):901-914
[8]  刘振武,撒利明,巫芙蓉等.中国石油集团非常规油气微地震监测技术现状及发展方向[j].石油地球物理勘探.2013,48(5):843-853??浏览
[9]  liuzhenwu,saliming,wufurongetal.microseismicmonitortechnologystatusforunconventionalresourcee&panditsfuturedevelopmentincnpc[j].ogp.2013,48(5):843-853??浏览
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[11]  grechkav,yaskevichs.azimuthalanisotropyinmicroseismicmonitoring:abakkencasestudy.geophysics,2014,79(1):ks1-ks12.
[12]  vavryukv.tensileearthquakes:theory,modeling,andinversion.journalofgeophysicalresearch:solidearth,2011,116(b12):b12320.
[13]  laytandwallacetc.modernglobalseismology.academicpress,newyork,1995.
[14]  jiaowj,davidsonmandsenaa.thematterofsize:onthemomentmagnitudeofmicroseismicevents.geophysics,2014,79(3):ks31-ks41.
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[16]  akikandrichardspg.quantitativeseismology(2ndedition).universitysciencebooks,2002.
[17]  孟昭波,杨丽华.地震勘探正演问题中震源机理的数值模拟[j].石油地球物理勘探.1990,25(1):45-52??浏览
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[19]  maxwellsc.microseismic:growthbornfromsuccess[j].theleadingedge.2010,29(3):338-343
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[23]  ?ílenyj,hilldp,eisnerletal.non-double-couplemechanismsofmicroearthquakesinducedbyhydraulicfracturing.journalofgeophysicalresearch:solidearth,2009,114(b8):b08307.
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