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简介：日本学者小泉顺子在泰国国家档案馆发现了20世纪早期关于客家的一些重要资料。在本文中，小泉顺子通过对这些资料的介绍和分析，向读者说明了客家在泰国和东亚、东南亚社会中比起其它族群（如潮州、广府），虽然人数相对较少，却扮演着十分重要的角色。

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简介：RegisteredandestablishedinThailand,theThai-ChineseInternationalTradePromotionCentreCo.,LtdisaservicecorporationinvestedjointlybytheChinaCouncilforthePromotionofInternationaltradeandtheThai-ChinesePromotionofInvestment

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简介：Forthetwo-linehybridricesystem,pollensterilityisregulatedbyrecessivegenethatrespondstotemperature.Therecessivegenecontrollingthermo-sensitivegeneticmalesterility(TGMS)isexpressedwhentheplantsaregrowninconditionswithhigherorlowercriticaltemperatures.Totransfertgmsgene(s)controllingTGMStoThairicecultivarsbybackcrossbreedingmethod,amalesterilelinewasusedasadonorparentwhileThairicecultivarsChaiNat1,PathumThani1,andSuphanBuri1wereusedasrecurrentparents.TheBC2F2linesweredevelopedfrombackcrossingandselfing.Moreover,thesimplesequencerepeat(SSR)markersweredevelopedforidentifyingtgmsgeneandthelinkedmarkerwasusedforassistingselectioninbackcrossing.Theidentificationlineswereconfirmedbypollenobservation.TheresultsshowedthesuccessofintrogressionofthetgmsgeneintoThairicecultivars.TheselineswillbetestedforcombiningabilityandusedasfemaleparentinhybridriceproductioninThailand.

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简介：ThelinkbetweenthecrustaldeformationandmantlekinematicsintheTibetanPlateauhasbeenwellknownthankstodenseGPSmeasurementsandtherelativelydetailedanisotropystructureofthelithosphericmantle.However,whetherthecrustdeformscoherentlywiththeuppermantleintheShan-Thaiterrane(alsoknownastheShan-Thaiblock)remainsunclear.Inthisstudy,weinvestigatethedeformationpatternsthroughstrainratetensorsinthesoutheasternTibetanPlateauderivedfromthelatestGPSmeasurementsandfindthatintheShan-Thaiterranetheuppercrustmaybecoupledwiththelowercrustandtheuppermantle.TheGPS-derivedstrainratetensorsareinagreementwiththeslippingpatternsandratesofmajorstrike-slipfaultsintheregion.Themostprominentshearzone,whoseshearstrainratesarelargerthan100×10^–9a^–1,isabout1000-km-longinthewest,trendingnorthwardalongSagaingfaulttotheEasternHimalayanSyntaxisinthenorth,withmaximumrateofcompressivestrainupto–240×10^–9a^–1.AsecondaryshearzonealongtheAnninghe-XiaojiangFaultintheeastshowssegmentedshearzonesnearseveralconjunctions.WhilethestrainratealongRRFisrelativelylowduetothelowsliprateandlowseismicitythere,inLijiangandTengchongseverallocalshearzonesarepresentunderanextensionaldominatedstressregimethatisrelatedtonormalfaultingearthquakesandvolcanism,respectively.Furthermore,bycomparingGPS-derivedstrainratetensorswithearthquakefocalmechanisms,wefindthat75.8%(100outof132)oftheearthquakeT-axesareconsistentwiththeGPS-derivedstrainrates.Moreover,wefindthattheFastVelocityDirection(FVDs)atthreedepthsbeneaththeShan-Thaiterraneareconsistentwithextensionalstrainratewithgraduallyincreasingangulardifferences,whicharelikelyresultingfromthebasalshearforcesinducedbyasthenosphericflowassociatedwiththeobliquesubductionoftheIndiaplatebeneaththeShan-Thaiterrane.Therefore,inthisregiontheuppercrustd