inferred英文

可疑是指形容一个人值得怀疑，不能完全信任。那么你知道可疑的英文单词是什么吗?下面我为大家带来可疑的英文单词和相关例句，供大家参考学习。可疑的英文单词1： suspicious 英 [səˈspiʃəs] 美 [səˈspɪʃəs] 可疑的英文单词2： dubious 英 [ˈdju:bjəs] 美 [ˈdubiəs, ˈdju-] 可疑的英文单词3： doubtable 可疑相关英文表达： 可疑分子 a suspicious character; 可疑行为 suspicious actions 可疑故障 suspected fault 可疑债务 doubtful debts 可疑账款 doubtful account 可疑英文单词例句： 1. Joseph watched a shady-looking bunch playing cards aboard a Mississippi steamer. 约瑟夫看到一群可疑的人在密西西比河的一艘轮船上打牌。 2. His best friend was killed by police under extremely questionable circumstances. 他最好的朋友在极其可疑的情况下被警察打死了。 3. He reported that two suspicious-looking characters had approached Callendar. 他 报告 说两个形迹可疑的人曾跟卡伦德接触过。 4. The police inferred that they found her behaviour rather suspicious. 警方暗示他们发现她行为非常可疑。 5. The report mentions the death of 18 people in suspicious circumstances. 那份报告提到18人死亡情况可疑。 6. Nottingham police last night found what they described as a suspicious package. 诺丁汉警方昨晚找到了他们声称的可疑包裹。 7. Detectives are appealing for witnesses who may have seen anything suspicious. 探员呼吁看到任何可疑情况的人进行举报。 8. Scotland Yard had assured him he was not under suspicion. 伦敦警察厅已经向他保证，他没有被视为可疑分子。 9. He warned the public to be vigilant and report anything suspicious. 他警告公众要提高警惕，遇到任何可疑情况都要报告。 10. Delegates evacuated the building when a suspect package was found. 发现可疑包裹后，代表们撤离了这座楼。 11. Police are investigating the suspected drug ring at the school. 警方正在调查这所学校的可疑贩毒团伙。 12. That claim is increasingly open to doubt. 那一说法越来越可疑。 13. The whole affair has been highly suspect. 整件事情一直都非常可疑。 14. Agents regularly rounded up suspected subversives. 特工定期围捕可疑的颠覆分子。 15. Manfred, you're a suspicious old devil. 曼弗雷德，你是个可疑的老家伙。

1. infer infect [in'fAkt] vt.传染，感染；影响...infer [in'f4:] vt.推论，推断...inference ['inf4r4ns] n.推断结果，结论；推论，推理，推断blog.163.com - 相关搜索 2. deduce 这是一组形近易混词。...deduce v.推断，推理，演绎。 - 相关搜索3. deduce from vt.演绎，推论，推断...deduce from演绎；推断...deduciblewww.bm8.com.cn - 相关搜索4. make of make believe 假装，假扮...make of 理解，推断...make up to 接近；巴结；向…求爱 - 相关搜索

An earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves. Earthquakes are recorded with a seismometer, also known as a seismograph. The moment magnitude of an earthquake is conventionally reported, or the related and mostly obsolete Richter magnitude, with magnitude 3 or lower earthquakes being mostly imperceptible and magnitude 7 causing serious damage over large areas. Intensity of shaking is measured on the modified Mercalli scale.At the Earth's surface, earthquakes manifest themselves by a shaking and sometimes displacement of the ground. When a large earthquake epicenter is located offshore, the seabed sometimes suffers sufficient displacement to cause a tsunami. The shaking in earthquakes can also trigger landslides and occasionally volcanic activity.In its most generic sense, the word earthquake is used to describe any seismic event—whether a natural phenomenon or an event caused by humans—that generates seismic waves. Earthquakes are caused mostly by rupture of geological faults, huge amounts of gas migration, mainly methane deep within the earth, but also by volcanic activity, landslides, mine blasts, and nuclear experiments.An earthquake's point of initial rupture is called its focus or hypocenter. The term epicenter means the point at ground level directly above this.

whatisearthquake?earthquakesdroppressuresthatcauselastingchangesintheearth'scrust.manyofthepeoplelivinginiranhadexperiencedanearthquake.whenwefeelsomethingviolentorsomethingslowlikerollingmotionoftheearthifweareatsleep,wewillwakeuporifweareathomeandwatchingtelevisionordrivinginthestreetwhenanearthquakehappens,wewillamaze.whatisthereasonforearthquake?whyfeelofearthquakesaresodifferentfromtheother?whatisearthquake?earhquakescausedroppingpressureandthesearetheearth'snaturalmeans.whileearth'splatesmovingintheoppositedirectionofeachother,agreatamountpressurewillimposetolithosphere.thelithospherebreakswhenthepressureisgreat.forexampleimagineyouhaveapencil.ifyougiveaforcetobothendsofityouwouldseathatpencilstoop.whenyougiveenoughforce,thepencilwouldbreakinthemiddlepart,andtheforcethatyouhadimposeditwoulddropping.theactionoftheearth'scrustisexactlylikethis.whentheplatesmove,theystressoneachotherandthemselves.whilethispressuresandstressesisgreatenough,thecrustwouldbreak.afterthecrustbreak,thepressurewilldecreaseasenergytmovesamongtheearth'slayersinformofwaves,andearthquakehappen.naturallyoccurringearthquakesmostnaturallyoccuringearthquakesarerelatedtothetectonicnatureoftheearth.suchearthquakesarecalledtectonicearthquakes.theearth'slithosphereisapatchworkofplatesinslowbutconstantmotioncausedbytheheatintheearth'smantleandcore.plateboundariesglidepasteachother,creatingfrictionalstress.whenthefrictionalstressexceedsacriticalvalue,calledlocalstrength,asuddenfailureoccurs.theboundaryoftectonicplatesalongwhichfailureoccursiscalledthefaultplane.whenthefailureatthefaultplaneresultsinaviolentdisplacementoftheearth'scrust,theelasticstrainenergyisreleasedandelasticwavesareradiated,thuscausinganearthquake.itisestimatedthatonly10percentorlessofanearthquake'stotalenergyisultimatelyradiatedasseismicenergy,whilemostoftheearthquake'senergyisusedtopowertheearthquakefracturegrowthandiseventuallyconvertedintoheat.therefore,earthquakeslowertheearth'savailablepotentialenergyandthermalenergy,thoughtheselossesarenegligible.todescribethephysicalprocessofoccurrenceofanearthquake,seismologistsusetheelastic-reboundtheory.themajorityoftectonicearthquakesoriginateatdepthsnotexceedingafewtensofkilometers.earthquakesoccurringatboundariesoftectonicplatesarecalledinterplateearthquakes,whilethelessfrequenteventsthatoccurintheinteriorofthelithosphericplatesarecalledintraplateearthquakes.wherethecrustisthickerandcolder,earthquakesoccuratgreaterdepthsofhundredsofkilometersalongsubductionzoneswhereplatesdescendintotheearth'smantle.thesetypesofearthquakesarecalleddeepfocusearthquakes.theyarepossiblygeneratedwhensubductedlithosphericmaterialcatastrophicallyundergoesaphasetransition(e.g.,olivinetospinel),releasingstoredenergy—suchaselasticstrain,chemicalenergyorgravitationalenergy—thatcannotbesupportedatthepressuresandtemperaturespresentatsuchdepths.earthquakesmayalsooccurinvolcanicregionsandarecausedbythemovementofmagmainvolcanoes.suchquakescanbeanearlywarningofvolcaniceruptions.arecentlyproposedtheorysuggeststhatsomeearthquakesmayoccurinasortofearthquakestorm,whereoneearthquakewilltriggeraseriesofearthquakeseachtriggeredbythepreviousshiftsonthefaultlines,similartoaftershocks,butoccurringyearslater,andwithsomeofthelaterearthquakesasdamagingastheearlyones.suchapatternwasobservedinthesequenceofaboutadozenearthquakesthatstrucktheanatolianfaultinturkeyinthe20thcentury,thehalfdozenlargeearthquakesinnewmadridin1811-1812,andhasbeeninferredforolderanomalousclustersoflargeearthquakesinthemiddleeastandinthemojavedesert.