海洋学报(中文版)
海洋學報(中文版)
해양학보(중문판)
ACTA OCEANOLOGICA SINICA
2015年
6期
58-69
,共12页
朱爱美%石学法%邹建军%张辉%吴永华%刘焱光
硃愛美%石學法%鄒建軍%張輝%吳永華%劉焱光
주애미%석학법%추건군%장휘%오영화%류염광
元素地球化学%黑潮%海平面%东亚季风%冲绳海槽北部
元素地毬化學%黑潮%海平麵%東亞季風%遲繩海槽北部
원소지구화학%흑조%해평면%동아계풍%충승해조북부
elemental geochemistry%Kuroshio Current%sea level%East Asian monsoon%northern Okinawa Trough
对 CSH1岩心全样沉积物样品进行元素地球化学分析,揭示了过去88 ka 冲绳海槽北部沉积物成分、水动力条件及陆源碎屑物质源区风化历史。冲绳海槽北部碎屑沉积物母岩主要以长英质为主,在 MIS 1期沉积物存在大量火山源物质。过去88 ka,沉积物源区风化程度较弱,但是自冰消期以来有逐渐增强的趋势。沉积物 Zr/Nb 比值表明在 MIS 1期和 MIS 5.1期水动力较为强烈,这与黑潮增强的时间一致,可能是指示黑潮强度的一个指标。冲绳海槽北部陆坡沉积物陆源碎屑贡献在低海平面时期显著增加,而在 MIS 1和 MIS 5.1期生源贡献显著增加。冲绳海槽北部沉积物成分变化明显受到黑潮和入海径流的调节,实际上受海平面和东亚季风的制约。
對 CSH1巖心全樣沉積物樣品進行元素地毬化學分析,揭示瞭過去88 ka 遲繩海槽北部沉積物成分、水動力條件及陸源碎屑物質源區風化歷史。遲繩海槽北部碎屑沉積物母巖主要以長英質為主,在 MIS 1期沉積物存在大量火山源物質。過去88 ka,沉積物源區風化程度較弱,但是自冰消期以來有逐漸增彊的趨勢。沉積物 Zr/Nb 比值錶明在 MIS 1期和 MIS 5.1期水動力較為彊烈,這與黑潮增彊的時間一緻,可能是指示黑潮彊度的一箇指標。遲繩海槽北部陸坡沉積物陸源碎屑貢獻在低海平麵時期顯著增加,而在 MIS 1和 MIS 5.1期生源貢獻顯著增加。遲繩海槽北部沉積物成分變化明顯受到黑潮和入海徑流的調節,實際上受海平麵和東亞季風的製約。
대 CSH1암심전양침적물양품진행원소지구화학분석,게시료과거88 ka 충승해조북부침적물성분、수동력조건급륙원쇄설물질원구풍화역사。충승해조북부쇄설침적물모암주요이장영질위주,재 MIS 1기침적물존재대량화산원물질。과거88 ka,침적물원구풍화정도교약,단시자빙소기이래유축점증강적추세。침적물 Zr/Nb 비치표명재 MIS 1기화 MIS 5.1기수동력교위강렬,저여흑조증강적시간일치,가능시지시흑조강도적일개지표。충승해조북부륙파침적물륙원쇄설공헌재저해평면시기현저증가,이재 MIS 1화 MIS 5.1기생원공헌현저증가。충승해조북부침적물성분변화명현수도흑조화입해경류적조절,실제상수해평면화동아계풍적제약。
Based on the analysis of major and minor elements in bulk sediments of core CSH1,we reconstructed the changes of sediment components,hydrodynamic conditions and weathering history in the provenance of terrigenous materials over the last 88 ka in the northern Okinawa Trough .The results show that the lithology of parent rock of the terrigenous detritus is felsic,and the volcanic detritus contributes significantly to the sediment components during MIS 1.Over the last 88 ka,the weathering in the provenance of terrigenous detribus is weak (WIP<60%) but gradually increases since the last deglacial period.The Zr/Nb ratio indicates the hydrodynamic condition was much stronger during MIS 1 and MIS 5.1 in the northern Okinawa trough,a potential indicator of the strength of the Kuroshio,which occurs synchronically with the intensified Kuroshio.The terrigenous contributions significant-ly increased during lower sea level,while the biogenic contributions showed high values during MIS 1 and MIS 5.1. The sediment components are regulated by the Kuroshio and the runoff in the northern Okinawa Trough ,which in fact are controlled by sea level and the East Asian Monsoon.