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1、IndexofRockMagnetism:FundamentalsandFrontiers(DavidJ.DunlopandÖzdenÖzdemir,1997.)296,299Aasanormalizingfactor[]非磁滞磁化率是Alternatingfiled(AF)demagnetization交变场退磁一个常用的校正参数299,332,436229-30,310-2anisotropy[]各向异性ofARM非磁滞剩磁的交变退磁229-30,290-1,296-30
2、0,configurational[]形状各向异性39-40,309,34092ofCRMorCVRM化学剩磁或化学粘滞剩磁的交变退magnetocrystalline[]磁晶各向磁372-4,379-81,387-90异性36-42,115-7,519-20ofhardVRM强粘滞剩磁的交变退磁275-6,454-5,magnetoelasticormagnetostrictive[]476-7[
3、]磁弹性各向异性或磁致伸缩各ofmultidomaingrains多畴颗粒的交变退磁256,290-1,向异性42-4,137,451301-6,358-9ofremanence剩磁各向异性484-8ofpseudo-single-domiangrains[]假单畴-单ofsusceptibility磁化率各向异性429-30,484-8畴颗粒的交变退磁305-6,340-1shape形状各向异性80,89-92,137,519-20ofsaturationisothermalr
4、emanence[]uniaxial[]单轴各向异性37-8,42-4,137,[`](SIRM)饱和等温剩磁的交变退磁451229-30,290-2,301-6,309,340-1,358-9anorthosite[]斜长岩419-20,511-14ofsingle-domaingrains单畴颗粒的交变退磁229-30,antiferromagnetism[`]反铁磁性289-92,3062
5、5,35-6ofTRM热剩磁的交变退磁229-30,256,290-1,306,340,Araiplot(seealsopaleointensitydetermination,Thellier389method)Arai图(也见于古强度测量,Thellier法)225ofweak-fieldandstrong-fieldremanences弱场剩磁和强archeomagnetism考古磁学423-4场剩磁的交变退磁(Lowrie-Fullertest)233,306-9,420authigenicminerals[
6、]自生矿物367-8,442,theoryof交变退磁理论229-30,289-91,301-6447-8anhystereticremanentmagnetization(ARM)[][`][]非B磁滞剩磁296-300,484-5AFdemagnetizationof非磁滞剩磁的交变退磁Barkhausen巴克豪森效应296-300,309,340discreteness[dɪˈskriːtnɪs]巴克豪森组件350-1grain
7、sizedependence非磁滞剩磁对粒度的依赖性jump巴克豪森跳变135,146,155-8,234,237,240,245,298-300,330-2,436262,265,276-7,336inmultidomaingrains多畴颗粒的非磁滞剩磁298,330volume巴克豪森体积234,245-6,262,276-7insingle-domaingrains单畴颗粒的非磁滞剩磁298,basalt[]玄武岩315,330lunar[]月球玄武岩511-4theoryof非磁滞剩磁
8、理论312-5subaerial[]]地表玄武岩404-14,466-9anhystereticsusceptibility[]非磁滞磁化率submarine[]洋底玄武岩268-70,392-4031IndexofRo