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1、第四章地球的年齡和地質(zhì)年代學(xué)TwoConceptionsofEarthHistoryCatastrophism(災(zāi)變說(shuō))Assumption:GreatEffectsRequireGreatCausesEarthHistoryDominatedbyViolentEventsUniformitarianism(均變論)Assumption:WeCanUseCauseAndEffecttoDetermineCausesofPastEventsFinding:EarthHistoryDominatedbySmall-scaleEventsTypicalofthePresent.C
2、atastrophesDoHappenButAreUncommon4.1相對(duì)地質(zhì)年代N.Steno地層層序律層序地層學(xué)方法W.Smith生物地層學(xué)方法標(biāo)準(zhǔn)化石時(shí)間短、演化快、分布廣地層的缺失-不整合(角度不整合、假整合)相互切割關(guān)系地質(zhì)年代表relativeageandabsoluteageRelativeage(相對(duì)年齡)-?Relativemeansthatwecandetermine?ifsomethingisyoungerthanorolderthansomethingelse.?Relativetimedoesnottellhowoldsomethingis,all
3、weknowisthesequenceofevents.?Forexample:?thesandstoneinthisareaisolderthanthelimestone.Absoluteage(絕對(duì)年齡)-?Absoluteagemeansthatwecanmoreorlesspreciselyassignanumber(inyears,minutes,seconds,orsomeotherunitsoftime)totheamountoftimethathaspassed.?Thuswecansayhowoldsomethingis.?Forexample:?Thesa
4、ndstoneis300millionyearsold.PKUTrashPitTHUTrashPitWhatcanwesayandlearnfromtheseexcavations?RelativeageoftrashlayersSimilarculturesmusthaveexistedinbothareasandlivedatthesametimeThetrashpitscontainsomecluestoabsoluteageRecognizeahiatus,orbreakinthedepositionalsequenceattheTHUsiteIngeology,we
5、usesimilarprinciplestodeterminerelativeages,correlations,?andabsoluteages.Relativeages-?PrinciplesofStratigraphyCorrelations-Fossils,keybeds,physicalcriteriaAbsoluteages-Radiometricdating.PrinciplesofStratigraphyStratigraphy(地層學(xué))=?thestudyofstrata(layers)intheEarth'scrust.LawsofStratigraphy
6、(地層學(xué)定律):1.OriginalHorizontality-sedimentarystrataaredepositedinlayersthatarehorizontalornearlyhorizontal,paralleltoornearlyparalleltotheEarth'ssurface.2.StratigraphicSuperposition-BecauseofEarth'sgravity,depositionofsedimentwilloccurdepositingolderlayersfirstfollowedbysuccessivelyyoungerlay
7、ers.水平地層相對(duì)地質(zhì)年代BreaksintheStratigraphicRecord---unconformity(不整合)AngularUnconformity(角度不整合)Disconformity(平行不整合、假整合)Nonconformity(非整合、不整合)不整合關(guān)系示意圖VariationinUnconformitiesStratigraphicClassificationTwotypesofstratigraphicclassificationareused,onebasedonphy