ISSN1009-2722`````MarineGeologyLetters`ݚလֹᇉ```2002,18(10)21i28໓ᅣщݼ:1009-2722(2002)10-0021-08俄罗斯大洋固体矿产资源调查研究进展许东禹(ౝ֛ݚလֹᇉ࣮෮,ౝ֛266071)ᅋ`ေ:介绍了俄罗斯的海洋多金属结核、铁锰结壳、热液硫化物和磷钙土资源调查研究活动概况和发展趋势。ܱՍ:海洋矿产;铁锰结壳;俄罗斯ᇏٳোݼ:P744```໓ངѓ്:A``2002୍4ᄅ20ᇀ25ರ,oݓ࠽ݚလঀӁՎࢨ؍ଽྙӮܞնလϰॶބՈ࣡ջ,ൈࡗູ߶ၰpᄝجઅථ഼cд֤Ѝईྛbجઅථ࿐ᆀᄝ50Ma;ֻ2ࢨ؍ູ٤ঔᅦࢨ؍(K1iK2,120j߶ၰഈؿі֥ં໓ބህีБۡսіਔ֒భݓ࠽80Ma),ܼٗؿტࠅቔႨ,ྙӮऍնࠅջ;ഈھਵთ֥࣮གྷሑބࣉᅚbགྷο҂ঀᇕٳֻ3ࢨ؍ູཌྟႵঔᅦࢨ؍,ྙӮ୍նလљࢺകטҰ࣮ۀঃބᇶေӮݔbϰॶ(K2iP3,80j26Ma);ֻ4ࢨ؍ູႵཌྟঔᅦࢨ؍,Ӂളնလᇏࠬ(26j0Ma)b1`؟ࣁඋࢲނބڶ᪦ࢲ॔նလؿᅚݖӱᇏྙӮਔห൹֥ܒᄯোiiሇߐ؎Ҫ,ૌ൞ઝൔ၇ՑྙӮ,֥ఃྙ1Ӯൈսնᇁ൞ኾઅࡀaພϢᎡൗaྍൗ,ພࡶ.1`նလঀӁሧჷྍൗ,ྍֻࡀbႮᇶщSIAndreev(ν֤ਙဵڏ)ࢺകਔᇏࡼӮঀ߃ٳӮ҂ࠩљ֥თ:щ֥ᆷ֝නམaჰᄵބଽಸ,ھщᇅႿջiջࠇസ(belt,Province)iთ(fieldࠇre-2000୍,ႮجઅථնလֹᇉঀӁ࣮෮щᇅbgion)iঀջ(orezone),ঀ(oredistrict)iঀھၛϰॶܒᄯંູᆷ,֝ၛֹᇉ୍սaܒᄯaܒᄯཌྷࠣఃؿᅚࢨ؍ູМࣟ,ѓൕਔํࢲ(oreknot)iঀbӦࠒํࢲނބࢲ॔οֹ౯߄࿐หᆘٳູ5(ࢲނބࢲ॔);iྊ߄(ॶሑ߄,ಙሑ߄);ݣࣁඋୃބඣ(သ߄iো:ڶNiCu(क़ঘυiक़০ஂؘ)aڶသ߄a߄aਠූaฏූa݁ූ);ݣঀCo(༱ຯ။)aڶMn(ਗ਼ݚன)aڶNiฏූiਠঀӦࠒ;ࢲࣖሑ฿ಖగඣކ;ࡏ(ਗ਼ݚன)aᇏ؇ڶMiCuiCo(ᇏလঀ೩bݚன)aCo(ଲလݚன)bھࡼնလؿᅚݖӱٳູ4۱ࢨ؍ᇏοඣ߄࿐ࢸ૫ࡼӁঀඣധ؍߃ٳູೂ:ֻ1ࢨ؍ູঔᅦࢨ؍༯ࠫ۱:ቋ֮ݣသҪ(LOM)ބฏූਢࢸധ؇(J2iK1,171j120Ma),(CDCA),ڶ᪦ࢲ॔ӁႿ500j3500mඣധ൬۠ರ௹؍,ڶNiMnࢲނ(ਗ਼ݚன)ٳ҃ᄝת:2002-08-08ቔᆀࡥࢺ:ྸתგ(1936i),ଳ,࣮ჴ,Ֆ൙ݚလֹᇉလݚੈၴ҆ڸ࣍(3900j4300m)bFeiMn࣮۽ቔ.Ӧࠒֹ֥౯߄࿐োა၂ק֥ඣധ(ֹ)ྙҪഈ
22MarineGeologyLetters`ݚလֹᇉ```````````2002୍10ᄅ֥ૡ్ܱ༢Ӂളਔࢲނaࢲ֥॔ࠢঀ,ࠧࢲނູํသ߄Ӯঀ༢ᇶေ൳֞ೂ༯ࠫ۱ၹٳ҃ᄝധݚჰ,طࢲ॔ᄵٳ҃ᄝݚބݚ֥॥ᇅ:Ӯঀჷࠣఃหྟބିჷ;Ӯঀݖӱൈbᄝᆜ۱նလᇏၘؿགྷ67ԩჹࣟ:20۱ॢဆ߄ࠏᇅ;ӮঀߌbӮঀᇉটჷॖٳູਆთ(fields)ބ47۱(areas),ఃᇏ13۱თো:၂൞ֹᇉൈ௹Ӊ௹(ࠫϤຣᇀඔతຣ୍)܂ބ41۱໊Ⴟလഈ,ᇶေЇওक़ঘυiႋ;ؽ൞؋௹(ඔతᇀඔϤຣ୍)܂ႋbՖ43Maक़০ஂؘӮঀთ(ڶNiCuiFeiMnঀ)aభषလϰॶؿളథ၍,Ֆ23Maభषਗ਼Ӯঀთ(ڶMnঀ)ބચᅽݚঀთ(ڶؿളᇛ௹ྟᄎ,ᄯӮਔํࢲނބࢲ֥॔҂᪦ࢲ)॔bᄝႆ؇လഈႵ6۱ঀთބ20۱ঀ;ളӉܒᄯބളӉࡗ؎૫bն༆လഈ2۱ঀთބ20۱ঀ,ఃᇏЇও4۱SLAndreeev֩ᄝݚလ߄࿐ބնလӮঀಣඣࢲ॔ঀbᆜ۱նလFeiMnӦࠒঀሧჷቔႨ၂໓ᇏิԛ,ݚလඣ߄࿐หᆘ॥ᇅބ႕ཙਈູ817ၡt,ఃᇏလᅝ80%֥ሧჷਈ,նਔํӦࠒӮঀቔႨ,ಪູնလඣҪඣ߄࿐ٳ༆လູ%,ႆ؇လູ%;طᄝնလሹջ(Ҫ)ᄯӮਔ҂ো֥ํӦࠒbၛNiaሧჷਈᇏ,ڶNiCuࢲނᅝ25%,ڶMnCuބCoᇶေჭູљ၇ऌ,ࡼํӦࠒ֥ᅝ%,ڶCuູ%b߃ٳູ5ᇕֹ౯߄࿐ো:ڶCoaᇏ؇ڶധݚ؟ࣁඋ߄(DPS)ᇶေٳ҃ᄝնလNiCu(NiCuiCoቆٳหᆘ)aڶNiᇏࠬᇠ҆aުனֹaࠃਚܡބࠅ৽ڸ֥࣍CuaڶNiބCo֩bڶCoࢲނބࢲ॔ಣඣࠃջഈb50۱ׅ֥߄ӁֹၘᄝնԛགྷႿඣധ500j600m֥ቋ֮ݣသҪഈ,֒လᇏ֤֞ಒಪ,طऍӮঀջᇶေٳ҃ᄝလᇏඣധնႿ3000mൈࡶࡶཨാbᇏ؇ڶNiCuࠬഈ,10۱Ӯঀջԛགྷᄝလᇏࠬഈb(%%)ํӦࠒᆰࢤӁԛႿฏූݚလਠہሧჷਈॖაֹཌྷឡૅbݚလਢࢸധ؇ᆭ၂֥Ӧࠒᇏ,طڶNiCuํਠہ֥ྙӮߌႵਆᇕ:ࠧ҂ࠃնшჸӦࠒᄵӁᄝฏූਢࢸധ؇ၛധֹbބݚ(ࠧଖུݚလ֛ഈ)bնшჸਠہٳնလᇏํӦࠒঀοაඣ߄࿐ٳҪܱ༢ॖ҃ႵರЧݚaࡆ০ڞୄaਗ਼iᇆ০ݚρaٳӮ3۱ቆ:᪦ঀ(%%,ᇏӈਈϏն০༆ρaଉઌۢaष௴ֹؗ֩bݚਠہ%%,ࢠڶ>%);ঀ(Ni+Cuն҆ٳ൞ܞӦࠒ,ᇶေٳ҃ᄝඣധཬႿູ%j1%,ӈਈ%%,ڶ>500m֥ݚഈ,ࢲ॔ሑ֥ᄵٳ҃ᄝնႿ%);ঀ()Ni+Mnູ33%j37%,Ni֥ඣധԩ,ᇏလݚಕ൞ਠہ֥ᇶေӁ+Cuູ%%;ڶMnູ35%jֹb֛ბਠہٳ҃ᄝလ֥ᠽਗ਼֛aնလ42%;Ni+Cuູ%%b֛aઔෳ၈ຐ֛ބႆ؇လ഼֥֏֛ഈbնလඣҪ֥Լᆰඣ߄࿐ࢲܒაຓটିਈၹ฿ಖగඣކ൞၂ᇕమᄝ֥ିჷሧჷ,Ⴕૡ్֥ܱ༢,ࠧაဝڕഝ֥࠱ࢫэ߄Ⴕૌᇶေٳ҃ᄝ۲նလնшჸ֥ഈbܱ༢,గީໂཟٳջ॥ᇅਔํӦࠒঀ֥ໂཟᄝщᇅoնလঀӁሧჷٳ҃pൈ,ႄႨਔٳ҃,ࢲݔնလᇏ95%֥ํӦࠒঀࠢᇏٳ҃50000؟۱ํࢲނބࢲ֥॔࠺,1200؟ᄝ35¢Sބ45¢Nᆭࡗֹ֥ջഈb۱ᅟ໊֥ധݚ߄aݣࣁඋୃࠣඣٚ૫֥նလඣҪᇏԼᆰٳջ֥ቋᇶေ֥ඣ߄࿐ࢸሧਘ,3000۱ਠہٚ૫֥࠺ၛࠣ20000૫൞ቋ֮ݣသҪ(LOM),ฏූਢࢸധ؇۱ࡽٚ૫֥࠺b(DCA)ބႵࠏؽသ߄݁Ҁӊധ؇(CDSiO2),ᆃᇕඣ߄࿐ٳջ॥ᇅਔํӦࠒঀ֥Լᆰٳ҃ބ`ํࢲނބࢲ॔ӮঀቔႨোbجઅථଲٚݚလֹᇉाฐ৳ކุ֥VMAnikeeva֩ಪູնလᇏѳቂჭ֥ӦࠒYubko֩ษંਔํသ߄ঀ֥ӮঀቔႨ,ಪࠏᇅ൞ඣӮቔႨbնလᇏํࢲ֥॔ํᇉ
ֻ18जֻ10௹````````ྸתგ:جઅථնလܥุঀӁሧჷטҰ࣮ࣉᅚ23൞ࣜݖࢋุ॒৬֥ӦࠒቔႨྙӮᄝݚࠎঀڶࠢٳ҃ᄝလक़ঘυބक़০ஂؘਆᆭഈ֥,ఃᇏCoaNiaMoaVބѳቂჭѩ҂൞؎ਚջᆭࡗބᇏႆ؇လݚனഈbํӦࠒᇶေၛ৫ঀ֥ྙൔթᄝႿࢲ॔ᇏ,ط൞ၛྙྙӮᄝФ݁ᇉiᅔᇉٸ೩ڭۂ֥ധݚჰၳܒ֥ྙൔࠁೆႿࢲ॔ᇏ֥bഈbঀ֥پ؇൞2j20kg/m2,ഒඔॖղ30ࣉೆնလ֥ѳቂჭ֥টჷ൞ֹോakg/m2bPtݣਈ҂,ູۚ()-610bڄӮᇉaდᇥᇉb൞,္҂ିஆԢࡽቔঀ(ਗ਼):Ӂᄝလᇏࠬၴ҆ڸ֥࣍Ⴈބಣࠃaࡽಷ၁ၛࠣࡽඣ႕ཙ֥ധ؇҂ն֥ݚனഈbঀ֥پ؇ᄝ5j20kg/m2ॖିྟbํࢲ॔ᇏPt֥ݣਈෛሢݚလඣധؿᇀ30j40kg/m2ᆭࡗ,οMn֥ݣਈॖٳູ2ളэ߄,ఃनݣਈູ10-6,൞ᄝളӁ۱োbCoބPt֥ݣਈ(֮Pt,๙ӈ֮Ⴟඣധٓຶଽᄹ֞()10-6,മᇀղ10-6)-610;طՖ3000mඣധषPtݣਈૼڶ᪦ঀ(ଲလ):ᇶေӁᄝလଲཁࡨഒ(֞)10-6bࢲ॔ᇏPtݣਈෛ҆χֹഈ,پ؇ູ20j30kg/m2ᇀ45kg/m2,ඣധ֥э߄ᇶေ൳֞ඣ߄࿐ၹ֥॥ᇅ,ࠧฏCoݣਈ൞%%,Pt֥ݣਈࢠ,ۚሱූਢࢸധ؇(CDCA)ބቋ֮ݣသҪ(LOM)10-6ᄹࡆ֞10-6b֥॥ᇅb᪦iঀ(༱ຯ။):ᇶေၛࢲ॔ྙൔӁجઅථ֥Anikieevaಪູնလބֹ฿ಖᄝӦࠒޓഒ֥ࡔ႗െі૫,ӁളඣധٓຶඣᇏPtބPbᇶေ൞ၛ੯֥ކྙൔథ၍,൞600j3000m,ቋᇶေ֥Ӂളඣധࢤ࣍ቋ֮ࠧၛ2--[PtCL4]a[PdC2L4]ྙൔథ၍,ᆃPt(2ݣသҪ(LOM)bCo֥ݣਈनູ%,ӈղ+)ބPd(2+)ߎჰູPt(0)ބPd(0),ॖି൞%%,ѳݣਈሱ()10ᄹᆃᇕࣁඋܥק֞ঀᇕ֥၂ᇕྙൔ,طPtބࡆ֞()10-6,ቋۚॖղ10-6bPdᄝํࢲ॔ྙӮݖӱᇏФܥק֞ঀᇕ֥ᇶေࠏᇅ൞་ڸቔႨ`ํࢲ॔ٳ҃ܿੰجઅථଲٚݚလֹᇉाฐ৳ކุ֥`ํӦࠒঀ֥ٳোMelinikovᄝࢺകလચᅽݚํࢲ॔Andreev(1994)֩۴ऌํӦࠒᇏᇶေ֥ቇฐࢲݔൈ,ฐษਔํࢲ֥॔॔ިaࣁඋݣჭ(MnaNiaCuaCo)ބϴളჭ(MoaLoaCeaਈඣധaֹྙࠣࠎᇉ֥ܱ༢b2001୍k/vAuaAgaPt)֥ݣਈ,ࡼݚလํӦࠒঀٳູ4oGelendzikp(۬৵ࠝक़ݼ)ᄝચᅽݚ֥ᇕো,ఃᇏభ3ᇕ൞ࢲނሑঀ,ӯֆҪٳ҃ᄝIOANݚഈյਔ7۱రቇbࢲݔіૼ,ࢲ॔ऎඣധ4000j6000mധݚχֹӦࠒі૫ഈbႵ4۱ളӉҪ:Ҫú-1(ພܞྍൗiᄪྍൗ)aࢲނپ؇၂Ϯູ5kg/m2,طپ؇նႿ5kg/m2Ҫû-2(ᇏaພྍൗ)aҪû(ᇏྍൗ)ބҪü(ۄᇗ)ൈႵ۽ြၩၬbֻ4ᇕো൞ํࢲ,॔(ഈྍൗiֻඹࡀ)b۱љဢഈߎु֞ҪRaᇶေٳ҃ᄝඣധ800j3000m֥ݚഈ֥ܥ(िൗiઔථห০ތൗ)ބRb(ພܞྍൗ)b7ࢲӦࠒބ࿉ᆭഈ,ࢲ॔ި؇ᄝ1j8m۱।ᇏႵ4۱।յ֞ࠎഈ,ࠎྟູࢉཌྷᆭࡗ,پ؇ᄝ50j90ᇀ300kg/m2ᆭࡗ(An-ᇗࢲࣖߧbٳ༅іૼݚฌԩ֥ࢲ॔ި؇dreev,1995)ބႵႨࣁඋݣਈनбོഈࢲ֥॔նބۚbAnikieevaࢺകਔ4োํӦࠒঀֹ֥౯جଲٚ৳ކุ֥TMKhoulapova֩ٳ༅߄࿐ބٳ҃หᆘbਔڶ᪦ࢲֹ֥॔౯߄࿐หᆘ,ѩቓਔࢲֹ֥॔iํӦࠒঀ(क़ঘυiक़০ஂᇉބ۽ြࡎބ߃bᄝ࣮ํӦࠒӮঀֹؘ):ऌNiބCnݣਈ,ॖٳູ3۱ো,ॖᇉߌބҐঀ่ࡱൈ,ᇶေॉ੮ਔ4۱໙ี:ݚቔູ۽ြჰਘ֥ቆٳ൞NiaCuaCoaMnbՎোָֹ(ྙݚָі૫؇aࢆੱ);ঀԵӦࠒߌ
24MarineGeologyLetters`ݚလֹᇉ```````````2002୍10ᄅ(ࢲ॔ٳ҃і૫ᇏֹྙaࢲ॔ٳ҃ٳۯӱഒӑݖ4cm;൞ࣁඋݣਈࢠ:ۚ%,؇aӦࠒڭۂбੱaࢲނ֥Ӂԛ);ঀെބࠎᇉ%,%bหᆘ(ࢲ॔ބࠎᇉ֥ܥࢲ؇aࠎᇉӮٳ);ඣߌࢲ॔ᇏႵݝቆٳ,หљ൞P2aO2ݣਈᄝҪඣ৯ሑbúᇏቋۚbP2aO2ᄝҪࢲ॔ᇏ֥नݣਈູູਔषؿᇅҐঀބԩඌ,ᄝလ%,ቋۚղ%;චҪࢲ॔(ҪúބҪચᅽݚ֥IOANݚഈࣉྛਔঀ߃ٳü)ᇏन%,ቋۚղ%b۽ቔbࣉྛ߃ൈ၇ऌਔ҂֥ҕඔ,ఃᇏቋᇶऌၛഈٳ༅ॖᆩ,Ֆࣜ࠶ٚ૫ॉ੮,Ҫބေ֥ҕඔ൞ࢲ֥॔ި؇(҂ཬႿ4m)ބ᪦ݣਈචҪࢲ॔ၹఃٳܼ҃,ࣁඋݣਈࢠۚ,طऎႵ(նႿ%)bषҐࡎᆴbՖ۲োࢲނٳ҃หᆘট,ुᄝݚঀԵো֥߃ٳ൞۴ऌঀุٳӱ؇টࣉߏֹྙഈٳ֥҃ࢲ॔ቋႵषҐࡎᆴbྛ,֥طঀุٳӱ؇൞Ⴈᅶཌྷ௩૫টಒק֥`ࢲނބࢲ॔ളӉൎ(Melinikoov,1995),ऌՎ,߃ٳԛೂ༯ࠫোঀbجઅථۚࡆ෬ֹᇉטҰ෮֥IAPulyaeva(1)ໃٳࠇັٳ֥ࢲ॔ڭۂ,ᆃུ০ႨളֹҪ࿐ٚم,ಒקਔ༆လݚֹྙࠫެ൞ฌࠇ؇ޓߏ,ܒӮᆜ۱ݚঀ֥ํࢲ֥॔6۱ളӉҪ:ૌ൞ພϢᎡൗ;ພ֥48%bܞྍൗiᄪྍൗ;ᇏiພྍൗ;ພࡶྍൗi(2)ᇏ؇ٳ֥ঀ,ܒӮඔॺ֥ն֥ࢲᄪᇏྍൗ;ᇏiພᇏྍൗ;ഈྍൗi۷ྍൗbط॔ϰॶbᆃᇕঀ໊Ⴟݚ֥פ૫ބ૫,ܒӮࢲ֥॔ളӉࡗ؎௹൞ᄪܞྍൗބᄪiᇏࡶྍᆜ۱ݚ47%֥ঀbൗbෲࣉطฐษਔํࢲ֥॔ളӉൎაܞݚလ(3)ۚ؇ٳ֥ঀ,ॖྙӮ֚െؐbᆃဆ߄ൎ֥ܱ༢,ಪູࢲ֥॔ᇶေളӉࢨ؍აಆࢲ॔ෞॶ֥նཬ҂ӑݖඔ,ࢲ॔ສສބ౯ݚ௹ཌྷؓႋ;طఃളӉࡗ؎௹ᄵაಆ౯ݚࠎᇉaֆ۱ࢲ॔ࠣӦࠒࠁᄝ၂ఏ,ၹطാಀ۽௹ཌྷؓႋbြၩၬbجઅථКٚݚလֹᇉाฐ৳ކุ֥VVચᅽݚࢲ॔၂ϮऎႵ4Ҫࢲܒ,ሱShilou֩ࢺകਔתလक़ঘ০υiक़০ஂؘ༯طഈູҪú-1aҪú-2aҪû-2ބҪü-3b༯2؎ਚջᆭࡗֹ֥ํࢲނളӉ୍սބളӉҪࢲܒᇁૡ,ਠݣਈ,ۚႵႨቆٳݣਈ֮,طഈੱٚ૫֥ྍሧਘ,ૌ۴ऌ٢ഝԋ߄െ,ࡼת2Ҫࢲ॔ܒᄯܥࢲ؇ࢠҵ,ႵႨቆٳݣਈۚbလݚனक़ঘ০υބक़০ஂؘ؎ਚջᆭࡗ֥ํ۴ऌࢲ֥॔ളӉҪඔ,ࡼࢲ॔߃ٳູೂ༯ࢲނ؎૫߃ٳູ8۱ջ:ջúiû,۷ྍൗiࠫো:Ҫ(úiûiü)aචҪ(úiüބಆྍൗ;ջü,ພᇏྍൗiഈྍൗ;ջý,ᇏᇏྍûiü)ބֆҪ(ü)bൗ;ջþބÿ,ᄪᇏྍൗ;ջĀބā,ᄪᇏྍൗࠇҪӈӁႿݚഈ,ᅝऌঀ֥63%,ࡶྍൗb۴ऌഈඍളӉҪൈս,࠹ෘਔࢲނ҂ࢲ॔ި؇ູ6j12m,ᇶေࣁඋݣਈٳљ൞Coջ֥ളӉੱ%,%,%;චҪࢲ,॔֒චҪູҪûބҪüൈ,Ⴕ۽ြၩၬ,ૌܒӮ`ํࢲނᄝӦࠒі૫Ќթࠏᇅঀ֥31%,ࢲ॔ި؇ູ,ࣁඋجઅථ॓࿐ჽݚလ࣮෮֥IPKuzinษनݣਈ൞:%,%,%bંਔလक़ঘ০υiक़ஂؘ؎ਚջᆭࡗචҪູҪúބҪüൈ,ᆃোࢲ॔ٳ҃ޓ,ᆺᅝთ֥ํࢲނളӉ୍սބࢲނᄝӦࠒі૫ഈᆜ۱ঀ֥2%bࢲ॔ި؇ູ,ࣁඋЌթ֥ࠏᇅbૌ۴ऌັุܞളٳ༅ࢲݔ,ࢣनݣਈ:%,MnཬႿ20%,Niൕਔ࣮ሱພྍൗ֞ᄪᇏྍൗ(%;ֆҪࢲ॔ᆺᅝঀ֥4%,ࢲ॔ި؇ޓ17Ma)ູ৵࿃֥ӦࠒҪ;طሱ17j1Maࡗ
ֻ18जֻ10௹````````ྸתგ:جઅථնလܥุঀӁሧჷטҰ࣮ࣉᅚ25ؿളთྟӦࠒࡗ؎bૌႻ۴ऌํࢲނᇏ2000୍,oଲٚݚလֹᇉݼpԯᄝն༆လᇏ֥٢ഝԋ߄െ,ಪູࢲނྙӮ֥ൈսᇶေ൞ࡶࠬטҰൈ,ᄝਚܡ༆ҧฌࢨֹ֥ᇏ҆ؿགྷਔྍൗbਸ਼ຓ,ૌႻקਔݚํࢲ॔ڭۂྍ֥ಣ၁༢oNeptuneBeardp(ݚപޱሰ)bު֥϶ჹလᅔӦࠒބࢲ॔ᇏ֥ັุ߄െ,টoProfessorLogachevpטҰԯ֩ᄝ20ݴՑטಪູᅔྙӮ֥ൈս൞ພࡶྍൗ,طํࢲ॔Ұൈ,ಒಪਔoNeptuneBeardpಣ၁ӆഈ֥նਈྙӮൈսᄵ൞ֻඹࡀbKuzin֩۴ऌํࢲނํࢲ֥॔թᄝbࠣࢲ॔ྙӮൈսა༯ڙӦࠒൈսഈ֥ҵၳބ 大西洋无名海山上的铁锰结壳Ӂሑิԛਔ၂ᇕࡌඪ,ಪູํࢲނބࢲ॔TTR-11ݼֻ3ݴՑ,ᄝն༆လ௮ฤݚᇔЌᄝӦࠒі૫ഈ֥ᇶေࠏᇅ൞,ႮႿࢤρބઔ֣ঘ֛ᆭࡗ֥ݚഈҐࠢ֞ํࢲ࣍ᇏૅֹᆑࠃջֹ֥ଽؿള఼ֹ֥ᆑ(M॔ބࢲނဢ,ѩؓھဢࣉྛਔࢲܒܒᄯaঀ>),֤ݚָӦࠒؿളᆒ,֕ѩФֹᆑࠃބ߄࿐ٳ༅,ቋުࡼ߄࿐ٳ༅ࢲݔ߂֞࢘߄ਔָ֥ҪඣԊሼਔӦࠒ,طбࢠᇗն֥ํၹሰഈ,Ֆᇏुԛྍਆսࢲ॔b֥࢘ࢲނФЌᄝჰֹb࢘ׄٳљ൞PaMnބFeݣਈ 塞拉里昂海山的铁锰沉积矿微量元素`လᆭຓఃݚთ֥ํӦࠒঀӁ地球化学 芬兰湾的铁锰结核جઅථ॓࿐ֹ౯߄࿐აٳ༅߄࿐࣮෮֥جઅථֹᇉ࣮෮ᄝٯধຖת҆ࣉྛਔ༢AMAsauinࢺകਔն༆လೖঘυݚഈֹ֥֥ᇉטҰ,ᇅਔํࢲނٳ҃bVAํࢲ,॔ᄝפഈႵӦࠒۂҪֹ֥ٚࢲ॔ިZhamoidaބAGGrigorievࡼٯধຖ֥ࢲނٳ؇ࢠЊ,طࠎഈ֥ࢲ॔ި؇ᄵި,ॖղ8jູ4ቆྙো,ѩႨ࠹ٳ༅مؓб࣮ਔ10cm,ࢲ॔ᇏFeaTiaCaaMgaToaNaaCraNi҂ো֥ࢲނᄝ߄࿐Ӯٳഈ֥ҵၳbݣਈაఃᄝ༯ڙെᇏ֥ݣਈႵᆰࢤ֥ܱ༢; 大西洋中脊铁锰沉积物طMnaZnaCoݣਈა༯ڙҪಏીႵહܱجઅථoථหঘࠉڏჽൖݼp(R/VAca-༢,ඪૼMnaZnބCo֥Ӧࠒѩ҂൳ࠎᇉ֥႕demicNikolaiStrachev)(1989)aoଲٚݚလֹཙbᇉݼp(Yuzhmorgeologia)(2000)ބoઅࡆ్ڏ࢝൱ݼp(ProfessorLogachev)(2001)֩טҰԯ2`ਠہᄝݴՑטҰᇏ,ᄝ13¢Nބઔঘٿ؎ਚջᆭࡗ֥ն༆လᇏࠬਚܡഈؿགྷਔํӦࠒbجઅථ॓࿐ჽݚလ࣮෮֥GNBaturinᄝoථหঘࠉڏჽൖݼpֻ9ݴՑטҰݖӱᄝં໓ᇏษંਔݚလߌؓਠہ߄࿐Ӯٳ֥ᇏ,ᄝਚܡ༆ჸႨຩҐ֥֞ํӦࠒ൞գ႕ཙbЊ֥ࢲ,॔ఃหᆘ൞Mn/Feбᆴ֮(),ັູฐษߌؓਠہჭӮٳ֥႕ཙ,Ֆਈჭݣਈ္ࢠ:֮Cuູ480-610,Niູ҂ߌᇏ౼၂༢ਙਠہဢ,ٳ༅ਔఃᇏ100-610,Coູ1600-610,Znູ530ᇶေჭބ35ᇕັਈჭbՖնшჸބჹလ-610,Pbູ180-6-610,Cdູ510,൞ֹׅ҂ӦࠒߌᇏҐࠢਔགྷսᇀພϢᎡൗ֥֥ն༆လᇏ֥ࠬඣӮํӦࠒ;ൈ,oٮնਈਠہဢbնшჸ֥սіဢ൞౼ሱغථણֹᇉ࿐ࡅݼp(GeologFersman)טҰԯବбaਗ਼aᇆ০aଉઌۢࡏ,҃ঞक़ݚֻ10ݴՑטҰൈ,ᄝਚܡഈؿགྷਔඣ߄࿐ބඣބέܞঘථరฅbՎຓߎՖӔ༷תρರЧݚ֥໓ၳӈ,ॖିᆣૼᆃؿტႵಣ၁༢,ުնބֹۚaೖঘυݚੈaᇏလݚಕބଲটᄝਚܡת༆ਆҧшჸഈؿགྷਔറႿ࿉ԅ֡လഈ֥ઔୄ༐ࠎݚഈҐࠢਔ၂ུဢᇏ֥߄ঀ,іૼਔಣ၁ࠃ֥թᄝbb
26MarineGeologyLetters`ݚလֹᇉ```````````2002୍10ᄅԢSiO2ࠣႵࠏᇉ൞Ⴈ၂Ϯ߄࿐ٳ༅ٚمඣറೆ֞ޓധԩၛྙӮಣ၁; گᄖ֥ඣ߄࿐ࣉྛٳ༅ᆭຓ,ఃჭ൞ႨICP-MSaICP-ބඣ໓ၳӈᆣૼಣ၁ᇸ֥թᄝ,ఃྙӮ֥AFSބჰሰ་൬ܻ௶مࣉྛҩק֥bٳ༅ࢲݔ໊ᇂ൞ᄝਚܡོ֥༆К؍; ᄝਚܡ༆ҧࢨࢣൕਔჭᆭࡗႵૼཁ֥ཌྷܱܱ༢,֤ૌֹഈ֥ӦࠒҪᇏ҆Ⴕಣ၁ঀᄑiߛํঀ,ᇗॖၛ߃ٳԛਆնჭቆކ:ෞ྇ࠇӮჭቆࣖെބFeသ߄bᄝ4۱טҰׄഈҐ֮ࠢ֞ކ҆ٳބํသ߄ቆކ,ުᆀ൞ਠہྙ໑ํӦࠒ;!ࠎഈ֥ಣ၁эᇉᇗࢲࣖቔӮᆭުВႿသ߄ߌൈࣉೆ֞ਠہ֥ՑളႨ֥ޒࠖაሙࣜཟ؎ਚႵܱ,эᇉ࿉ބᣃቆٳbֻ1ቆЇওSiO2aAl2O3aK2OބTiO2aᢡᇏ֥߄ঀ߄֩ᆰࢤіૼਔಣ၁ࠃ֥LiaRbaCsaBeaGaaHtaNbaTbaThބZrbֻ2թᄝ;∀۴ऌၛഈ࣮֥ࢲݔॖၛҩ,ਚܡ༆ቆႮն҆ٳݖ؈ྟӮঀჭቆӮ,ࠧCoaCuaК҆ࠎބࢨֹ֥ഈ҆૫(12¢£j13¢N,NiaMoaPbaVބZnၛࠣັਈჭAsaBiaCda44¢£¢7£W)൞ॶሑ߄ቋႵჹࣟSbaSnaTeaTlaW;൞,ު၂ቆ֥၂҆ٳჭ,ֹ֥bหљ൞MoaCdaVބZnॖၛᄝသ߄ބߎჰਆ 现代热液成矿作用的新类型——Rain-ᇕߌॖၛؿളӦ,ᆺႵSrބP2O5ܱbow—热液活动场༢ޓૼಒbBatumษંਔ۲ᇕჭᄝਠہᇏجઅථ॓࿐ݚလ࣮෮֥YABogamov֥ٳ҃หᆘ,၂Ϯࡏਠہᇏ༎ჭݣਈࢺകਔᄝ1997୍༱,ᄝն༆လᇏࠬ36¢NԩྍཬႿჹလਠہ,طUބRtᄵڶࠢႿࡏਠؿགྷਔRainbow(ґޞ)ಣ၁ࠃӆbᆃᇕಣ၁ہbࠃაഘ໕ཌྷϴള,ԛགྷᄝᇠྏࡽٜaؿളഘ໕߄ቔႨ֥ঔᅦࠬ؍ഈbᆃোಣ၁ࠃ3`ॶሑ߄ӆࠣఃಣ၁Ӧࠒაൗࢸਚܡ༢֥ఃಣ၁नႵྸ؟ཌྷ,ׄ൞Ⴕၛ༯၂ུఃหᆘ: აഘ໕ॶϴള֥ۚ໑ಣ၁߄Ӧࠒऎ`ն༆လᇏࠬ߄ႵZnބCuiZnঀ߄ቔႨ;൞CoބNiݣਈ 马拉松断裂带(Marathonfracturezone)ޓۚbPtݣਈбఃಣ၁֥߄ۚ၂۱ඔ块状硫化物ਈࠩbRainbowಣ၁ӆ֥ಣ၁߄ᇏݣႵ᪦جઅථֹࠞݚလֹᇉॉҳ֥ؒVBeltenevߛํঀބᆌঀ,طᆃᇕঀؓൗࢸਚܡ༢֩ࢺകਔھॉҳؒაКٚݚလֹᇉाฐ৳ކุఃֹ֥ಣ၁ঀটࢃ൞٤ׅ;֥ Rain-০ႨoLogachev࢝൱ݼpԯֻ2ݴՑᄝն༆လbowಣ၁֥߄ᇏ໊֥Ӯٳ္Ⴕུҵᇏ֥ࠬ13¢j18¢Nᆭࡗਚܡ؍ഈ֥טҰӮݔbၳ,ࠧھ߄ᇏS໊ݣਈ൞+ªᇀ+ھטҰ֥ଢ֥൞ࢣൕགྷսބܞսಣ၁ࠃ,ಁª,طᄝఃਚܡ༢֥߄ᇏᄵູק߄֥ჹࣟbטҰਔ4۱,ׄఃᇏ၂۱ט+ªᇀ7ª,न3ªj5ª; აఃֹҰ໊Ⴟઔঘ؎ਚջၛК20kmԩ֥12¢48£ཌྷб,Чಣ၁ࠃ֥֮໑ಣ၁ᇉڶݣCuaj13¢04£Nބ44¢44£j45¢00£Wᆭࡗ,ᆃᄻႮNiބCo;!Чಣ၁ࠃ֥ಣ၁ӦࠒބಣoGeologFersmanpݼֻ10ݴՑބoYuzhmor-၁ಷ၁ᇏݣႵᄝഘ໕߄ݖӱᇏݚඣაӑࠎྟgeologiapݼބoAtlantispݼטҰԯᄻטҰؿགྷཌྷቔႨطӁള֥CH4ބଖུെႲฏ๑߄ކਔඣ߄࿐ބඣ໓ၳӈboProfessorLogach-;∀ᄝЧಣ၁ࠃഈି֞ਆোۚ໑ಣಅerpݼԯֻ20ݴՑטҰࢲݔ֤ԛਔೂ༯ࠫ۱ࢲoޑՔpbֻ1োoޑՔp൞ᄝਚܡջഈྙӮં: טҰܒᄯiֹྙหᆘ൞ၛࢤ࣍ሇߐ؎֥ׅ֥Ք,൞Ⴎࠞն֥ڜ৯ቔႨطӁളਚջູ༵थ่ࡱ֥,ᆃྙӮਔ၂༢ਙཌሑܒ֥ഈശ֥ಣ၁ྙӮ֥ಣ၁߄ܵ;ֻ2োᄯބॶሑܒᄯ,ܒᄯࠃ఼ਛ,ᆃᇕሑঃ֤ݚoޑՔp൞ۚ໑ಣ၁χֹࠇಣੀॠ,ᆃѩ҂
ֻ18जֻ10௹````````ྸתგ:جઅථնလܥุঀӁሧჷטҰ࣮ࣉᅚ27Ӂളಣ၁ഈശ,ط൞ခሢָ࣍Ҫቓඣ၍bଢҰ௹ࡗྍؿགྷ֥oLogachevûpॶሑ߄భ,ֻ2োoޑՔpᄝఃಣ၁ࠃߎໃֹ֥౯߄࿐หᆘbھॶሑ߄֥หᆘ൞֮Б֡;#Rainbowಣ၁ࠃ֥ಣ၁ᇏڶݣH2ݣ၂Ϯն༆လᇏࠬ࿉ᇏӈႵ֥ഘ໕,ބCH4,طCoݣਈޓ,ۚᆃᇕགྷའᄝఃಣطႰ(U)ݣਈหљۚbЧ߄ᇏݣႵ৭၁ߎીႵმbౝႰঀ,ၛ౯ሑྏჵܒᄯ৵ࢤႿခሢྊBogodanovಪູRainbowಣ၁ࠃಣঀaߛঀࠣߩঀຓ҆шࢸٳ֥֑҃Ϣെഈ,၁Ӧࠒ֥ഈඍหᆘ൞ႮႿఃྙӮݖӱбఃطᆃᇕঀቆކᇏӈݣႵሱಖࣁbಣ၁߄ಣ၁ࠃӉ֤؟طᄯӮ֥bᇏԛགྷ৭ౝႰঀᄝଖᇕၩၬഈࢃ൞ఘࣂֻ 大西洋中脊岩石类型与热液活动Ցؿགྷbݖಀ,ႵБ֡ඪᄝն༆လᇏࠬTAG؎جઅථКٚݚလֹᇉाฐ৳ކุ(VNIIO૫ഈ֥߄ᇏUݣਈᆺႵ4010-6(DJKeanologia)֥AITrukhalev֩ᄝં໓ᇏิMiller,1998),ॖ൞Logachevûಣ၁߄ᇏԛ,ն༆လᇏࠬႵਆᇕെো:ഈູ҆ࠅiؿགྷႰ(156010-6)a᪔(1510-6)aࣁ(50Ӧࠒቆކ,༯ູ҆ܞэᇉ֥ߩӉiӑࠎ10-6)aၿ(10-6)ݣਈޓۚ(MPྟቆކ,აՎཌྷႋ,ॖၛಒקԛਆ۱ӮঀቔႨTorokhovet2001),ඪૼഈඍ҂ཌྷಸჭ൞ֹဆ߄֥ࢨ؍,ࠧնလЧദ֥ພኾઅൗiྍളսᖧӮၹ֥bࢨ؍ބభնလ֥భݥࡀiཁളდࢨ؍ 大西洋中脊硫化物中贵重气体的同位ݚလࢨ؍֥ࡽ֥іགྷྙൔ൞࿉ۂ素——矿液来源的指示剂Ҫaܛ৫ࠅaaߩੳࠣ৬࿉Ե(෮໌ಆ්ֹᇉ࣮෮(VSEGEI)֥EMPra-ࠅiೆߩੳi࿉ቆކ)bsolov֩ࢺകਔն༆လᇏࠬLogachev-1aLo-ߩӉiӑࠎྟቆކܼٗٳ҃ᄝਚܡagachev-2ބRainbowঀโ֥߄֥HeaVeaሇߐ؎Ҫބն༆လᇏࠬࠬ҆აሇߐ؎ҪࢌࢤջAraKrބXe֩గุ໊,࣮ࢲݔіૼ,߄ഈ,ఃॺ؇ղඔϤ,Լᆰި؇ղ2j3km,࿐ࠃն֥గุࠎЧഈ൞ֹ॔Ӯၹ,֥طHeെႮߩӉi්ӉaՈํঀߩӉaߩӉބAr໊ሧਘіૼᄝঀ၁ྙӮݖӱᇏֹᖧa්ӉaᣃᢡߩӉބᣃӉቆӮbగุؿ္ҕࡆਔ၂҆ٳbնਈሧਘіૼႮߩӉiӑࠎྟܒӮ֥ 大西洋中脊上的汞ֹᖧބ༯ֹ॔ᄝെಁഈശݖӱᇏࣜਔگᄖجઅථ॓࿐ჽঀԵaെaঀބֹ౯߄࿐֥эᇉቔႨݖӱb࣮෮֥NAOzerova֩ሸކࢺകਔն༆လᇏಆބٳ֥ঀ୍໊սٳ༅ࢲݔіࠬ߄ᇏ܈֥ٳ҃หᆘ,ᆷԛѢ֛ބغૼ,ߩӉiӑࠎྟቆކྙӮႿభݥࡀiಕ֛֥လָ߄aӦࠒބࠅᇏ܈ݣਈཁളდ,ᆃোെቆކॖაն༆လᇛຶ֥٤ᇝ٤ӈٳbݚָӦࠒᇏ܈ݣਈቋۚᆴԛགྷႿࠣଲૅ֥െቆކཌྷбࢠ;ၹՎॖၛ؎,ᄝնޣᅔބํࢲ,॔طؓࡽটࢃႵ2ቆ:၂༆လᇏࠬധ҆ॖିᅳ֞োරႿଲૅϘ༆֥Fea൞Мࣟᆴູn10-6%ᆀ,ؽ൞܈ݣਈᄹնູnMnaNiaCraPGE(ѳቂჭ)ބ֩ঀԵbൌ࠽-510%jn-410%,ഘ໕ᇉӑࠎྟᇏ֥܈ഈ,ᄝն༆လᇏࠬ؟ԩၘࣜؿགྷႵՈํঀ,طݣਈࢠ,֮ݣࣁඋӦࠒᇏ܈ݣਈб߄֮ᄝն༆လᇏࠬӑࠎྟെᇏࣜӈ֞Ղᣃᢡ֤؟,൞նႿֹ॔नᆴ(10-6%),ః(ӈაߩെϴള),ႮՎॖၛҩᄝն༆လनᆴູ10-5%,གྷսݚလ߄ᇏ܈ᇏࠬॖିթᄝݣѳቂჭ֥Ղᣃᢡቆކbݣਈູ5-610%-610%,߄ᇏ܈ 块状硫化物中的铀及放射性同位素ྊaᆭࡗႵᆞཌྷܱܱ༢bVNIIOkeanologia֥MPTorokhovࢺകਔoProfessorLogachevpݼטҰԯֻ7ݴՑט
28MarineGeologyLetters`ݚလֹᇉ```````````2002୍10ᄅ 大西洋海底与蛇纹岩相关的块状硫化ਆ۱҆টປӮb॓࿐ჽݚလ࣮෮ᇶေڵᄳ物中高温出溶构造ࠎԤ࣮;طሱಖሧჷ҆ᄵᇶေڵᄳႋႨ(ሧجઅථ֥NMozgova֩ฐษਔն༆လ҂ჷ)࣮,ၛؿགྷބࡎྍঀԵሧჷbֹ߄֥ࢲܒܒᄯหᆘࠣఃა߄ྙ॓࿐ჽݚလ࣮෮(IO,RAS)ᇶေ൞০ႨӮ୍սaࠃ఼؇ࠣӮඃ؇֥ܱ༢bෲૌ࣮֥ധమఖ(ष൞ႨoPiscesp,Ֆ1987୍षႨֹ൞: Logachev-1ঀ(14¢45£N),ྙӮ୍oMirpݼധమఖ)࣮ਔလބն༆လഈ14սቋ(ղ),གྷၘࠫެ๔ᆸࠃ; ԩಣ၁ࠃӆ(ֹ)ࠣޱν֤ڶवလ֥ࠬݚRainbowঀ(36¢14£N),ྙӮ୍սႵэ߄(༆aࡆ০ڞୄຖ֥ܨઔථனֹa༆ଲလູ҆22j23ka,ᇏູ҆),ఃགྷս֥ଖུݚთބն༆လᇏࠬഈ֥4۱ֹ,ᇶေࠃ఼؇ቋն; Logachev-2(14¢43£22¤N),ቋଢ֥൞བྷ༥࣮߄ӮঀቔႨbଢభ,॓࿐ჽ୍(ᆺႵ),གྷᄝ҂ࠃbෲૌᄝ҂ݚလ࣮෮ᇶေᄝRainbowaLuckyStriktބֹಣ၁߄ঀุᇏؿགྷਔ֩ᇠܞϘঀԛಷLogachevಣ၁ӆഈࣉྛ࣮bࢲܒaሱಖࣁiഢԛಷࢌളܒᄯބྊঀiߛሱಖሧჷ҆(MNP)ᄝתလݚੈঀԛಷࢲܒbھં໓֥ቋުࢲં൞o߄֥(EPR)0¢j13¢Nބ20¢j22¢Sٓຶଽࣉྛਔն҂ࢲܒބঀӮٳ౼थႿ߄Ӧࠒ୍սaთטҰ,ᄝఃК҆ؿགྷਔ6۱ྍ֥߄ঀࠃ఼؇ၛࠣӮඃ؇pb߄ބ၂༢ਙ؎֥ಣ၁ࠃׄb80୍սष֥ն༆လᇏ֥ࠬטҰଢభಯ`جઅථᄝնလಣ၁߄ӮঀቔႨٚ૫֥࣮Ӯݔᄝࣉྛᇏ,ᆃࣉྛਔ࣍20۱ݴՑ֥טҰbᄝն༆လᇏࠬᇠ҆12¢j19¢Nބ21¢j29¢Nٓຶ``(1)جઅථܱႿնလಣ၁ቔႨ֥࣮Ⴟ50j100kmॺջଽࣉྛਔ1100000ބ120ൗࡀ60୍սᇏ௹,ѩֻ1ՑՖလҐࠢ200000б২Ԅֹ֥ᇉֹ౯טҰ,טҰཛଢ֞ݣࣁඋӦࠒ(Skornyakova,1964)bЇওֹྙaֹՈaݚလaݚလ߄࿐aҧೡല(2)ᄝੂ୍ս,جઅථࣉྛਔ၂༢ਙॉବa൪aᅶཌྷބֹᇉҐဢ֩bҳࠃ,࣮ਔလބႆ؇လᇏֹ֥֮ࠬࣜݖטҰ,ၘಒקԛ10۱ྍ֥ॖି֥ಣ၁໑Ӧࠒ,ೂݣࣁඋӦࠒބಣ၁ࢲ॔ၛࠣಣࠃӆ(28¢40£j28¢48£Na27¢05£j27¢10£Na25¢ඣၳӈ(Lisityn֩,1976,1979)b25£j25¢33£Nބ16¢07£j16¢09£N൞ቋႵ༐ຬ(3)1979୍,ۚ໑߄ӮঀቔႨ֥ؿགྷֹ֥);ؿགྷਔྍ֥ಣ၁߄Logachev-՜ࣉਔᆃোӦࠒ֥טҰބ࣮b1aLogachev-2ބ24¢30£Nۚݣ֥߄ঀ(4)80୍սԚष,جઅථषᅚਔնܿଆ߄ׄ;ᅶཌྷބຩҐࠢ֞Auݣਈޓ֥ۚဢb֥նလॶሑ߄֥טҰbᇶေႮሱಖሧჷ҆ؓᄝTAGֹಣ၁౭ഈҐ֥ࠢဢބ༵భ(MNP-ᇶေႮPMGRE,VNIIOkeangeologia,ؿགྷ֥SnakePitಣ၁ࠃࣉྛਔབྷ༥֥SevmorgeoቆӮ)ބجઅථ॓࿐ჽݚလ࣮෮࣮b
úABSTRACTSINTEGRATEDEVALUATIONOFMARINEGEO-ENVIRONMENTINDAPENGBAYXIAZhen(GuangzhouMarineGeologicalSurvey,CGS,Guangzhou510760,China),2002,18(10):1i5In2001,,-environmentinDapengBaywasintegratedandanalyzedonthebasisofseafloormor-phologyandrelief,,:marinegeo-environment;integratedevaluationDIVISIONOFMARINERESOURCESANDFUNCTIONSOFDALIANCITYMIAOFeng-min,LIShu-yuan,JIAOYi-ping,YUYong-hai,YANGXin-mei,ZHANGYong-hua,MIAOLi-juan,WANGQuan-ming(TheStateMonitoringCenterofMarineEnvironment,Dalian116023,China),2002,18(10):6i12AfterathoroughsurveyofDaliannsmarinenaturalenvironment,naturalresources,developmentsituationsandpotentialproblemsandanintegratedanalysisoftherequestsofregionaleconomicdevelopment,wedemarcatedmarinefunctionareasinseawatersofDalianCityandadjacentre-gionsandmaderelevantsuggestionstooperatethefunctionareas,inordertoscientificallyandreasonablydevelopandutilizemarineresources,controlandguidemarine-useorientation,protectmarineenvironment,promotesustainabledevelopmentofmarineresourcesandregionaleco-nomics,:marinefunctiondivision;importantseaareas;dominantfunction;managementmea-suresRESEARCHDEVELOPMENTOFRUSSIANOCEANICSOLIDMIN-ERALRESOURCESXUDong-yu
û(QingdaoInstituteofMarineGeology,CGS,Qingdao266071,China),2002,18(10):21i28Inthispaper,investigationsanddevelopmenttendencyofmarinepolymetallicnodules,ferroman-ganesecrusts,,andtookgeologicages,-velopmentintofourstages:thefirstwasdisorderedspreadingstage(J2-K1,171j120Ma)whentheancientoceanicplateandmagneticstaticzonesformed;thesecondwasanon-spreadingstage(K1-K2,120j80Ma)thatsawextensivelydevelopedvolcanism,asaresultofthat,greatvolcaniczonecameintobeing;thethirdwaslinearandorderedspreadingstage(K2-P3,80j26Ma),duringwhichyoungoceanicplatewascreated;andthefourthwasanorderedandlinearspreadingstage(26j0Ma)-callyclassifiedintofivetypes,namelyNi-Cu-richtype,Co-richtype,Mn-richtype,:marinemineralresources;ferromanganesecrusts;RussiaONSUBMISSIONOFMANUSCRIPTSINMARINEGEOLOGYTOFOREIGNSCIJOURNALSXUEChun-ting(QingdaoInstituteofMarineGeology,CGS,Qingdao266071,China),2002,18(10):32i34ItispopularintheEuropeancountries,,accordingtotheregulationthatallinternationaljournalsdonotpublishpapersthathavebeenpublishedonthejournalsinChinese,,whenyougetaseriesofdatayoushouldmakearrange-ment:,,:SCIjournal;contributors;publishing;internationaljournal
