专业外文参考文献

专业外文参考文献

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1、51,Precambrianmagnetite,hematiteandmagnetiteconstructioncausesTM.HanUnitedStatesPreparationofmorethanthreehundredpiecesofopticalfilms,beforeandafteroxidationweresignificantlyJiaomirrorBianobserved.TheserockswerecollectedfromthePrecambrianironformationsinthefollowing:1)

2、BiwabikUSALakeSuperiorregionmesabiregion,IronwooGobebicareaandNegauneeMarquettareaandotherplaces.2)LabradorTroughofQuebec,CanadaandAlbaneSokomanLakeareaTemiscamie.3)BrockmanHamerslayregionofWesternAustralia.4)Kuruman,SouthAfricaCapprovinceofTransvaalSupergrouparea.Thei

3、ronformationisessentiallyaccompaniedmainlybychertveins,saltandcarbon-layeredmagneticironoresiliconSuosaltcomposition.Hematitemayhave(containinglessthanmagnetite)maybenone,oroutputintheformofmagnetMinesymbiosis,oroccasionallyirregularenclavesFu.Lostamongstoredinthemagne

4、ticmine.Thefollowingobservationsindicatespecialcauseoxidationplaysakeyroleintheproceduresusedinthestudy:1,astablehematitephaseremainsunchanged.2,mostofthemagnetitestructurealongtheedgeofthepackageearlyexistenceofoxidation,ratherthancleavagesurfaceoxidationofmagnetiteal

5、ongtheedgesoftheseinclusionscanbeseenasearlyhematite(aftermagnetitehematiteillusion),includingmorphologyandthepresenceofresidualhematite(causedbyoxidationbeforeusingtheprogram)toillustratethispoint.3,theearlypresenceofhematiteandmagnetiteorearlygenerationsuccessionorin

6、termittentlyappeartoincreasewiththeproliferation.4,beforemagnetiteformation,someofthehexagonsand第1页diamond-shapedmorphologyduetothepresenceofearlyovergrowthandgrowth(possiblyself-generated)andchange.5,mostoftheearlypresenceofhematiteinclusionsmostlydisorderedarrangemen

7、t,butnearlyhorizontalorientationZheyinotuncommon.6,intheareaofirontobuildsomeofNegauneeclasticlenses,themagnetitedebriscontainingtitaniferousmagnetiteandchromitemagnetiteasacoregrowth.Accordingtotheaboveobservationscanbeenvisaged:A,themajorityofbothnativehematitemayals

8、obeformedduringdiagenetichematitemaybethroughdepositionorafterdepositionofFe(OH)immediatelyfromdehydration.Mightalsob

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