冲绳海槽岩浆物理化学性质及其地质意义

黄朋; 李安春; 胡宁静

冲绳海槽岩浆物理化学性质及其地质意义

1.
中国科学院海洋研究所中国科学院海洋地质与环境重点实验室, 山东青岛 266071
2.
国家海洋局第一海洋研究所, 山东青岛 266061

基金项目: 国家自然科学基金资助项目(40606021);中国科学院知识创新工程重要方向资助项目(KZCX3-SW-223)

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出版历程
- 收稿日期: 2007-04-17
- 修回日期: 2007-09-13

The physico-chemical features and their geological implications of magma in the Okinawa Trough

1.
Key Laboratory of Marine Geology and Environment of Chinese Academy of Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.
First Institute of Oceanography, State Ocean Administration, Qingdao 266061, China

摘要

摘要: 借助冲绳海槽火山岩地球化学分析结果,讨论了海槽不同区段岩浆的温度、压力、密度和黏度等物理化学参数,以确定海槽岩浆的物理性质及其对海槽不同区段岩浆演化过程的影响.海槽北段的岩浆相对于中段表现出高压力、低温度的特征.由于海槽岩浆挥发分含量较高,北段岩浆的密度和黏度要高于中段的.但总的来说,海槽岩浆具有低密度、低黏度的特点,因此岩浆更容易穿透岩石圈,而且有利于岩浆结晶分异作用的进行.对海槽岩浆相对运移速度的研究显示,在外部条件及含水量相同的前提下,在海槽中段岩浆上升速度要大于北段的,这从岩浆物理化学性质的角度解释了为何海槽中段火山活动要强于北段的.
- 冲绳海槽 /
- 物理化学参数 /
- 岩浆
Abstract: On the basis of geochemical data of volcanic rocks,the variety of physo-chemical parameters,including temperature,pressure,density and viscosity,was studied to underst and features and development of magma in the Okinawa Trough.The following conclusions were obtained:(1) the mag maunder the northern Okinawa Trough held higher pressure and lower tem perature than those of magma under the middle Okinawa Trough;(2) the magma of the northern Okinawa Trough had higher value of density and viscosity than that of the middle Okinawa Trough because the magma enriched volatile;(3) the low density and viscosity of magma under the Okinawa Trough were of advant age topent rate lithosphere and played fractional cry stallization;and(4) under the same environmental conditions and water content,the uplifted velocity of magma in the middle Okinawa Trough was higher than that in the northern Okinawa Though.It could explain why magmatism in the middle Okinawa Trough was more drastic than in the northern Okinawa Trough.
- Okinawa Trough /
- magma /
- physo-chemical parameters

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参考文献(27)

彭澎,翟明国.关于弧后扩张机制的新看法[J].世界地质.2002,21(1):1-8.

林美华,李乃胜.西菲律宾海中央断裂带地貌学研究[J].海洋地质与第四纪地质,1999,19(1):39-44.

SLEEP N,TOKSOZ M N.Evolution of marginal basins[J].Nature,1971,133:548-550.

金翔龙,喻普之.冲绳海槽的构造特征与演化[J].中国科学(B辑),1987,2:196-203.

MIKI M.Two-phase opening model for the Okinawa Trough inferred from paleomagnetic study of the Ryukyu arc[J].Journal of Geophysical Research,1995,100:8169-8184.

HSU S K,SIBUET J C,SHYU C T,et al.A note on the tectonic features and volcanism of the southern Okinawa Trough[C]//International Conference and SinG-American Symposium on Tectonics of East Asia.Chungli,Taiwan,1997:88.

HIRATA N.Report on DELP 1988 cruises in the Okinawa Trough:Part 3.Crustal structure of the southern Okinawa Trough[J].Bull Earthquake Res Inst,Univ Tokyo,1991,66:3-70.

江为为,刘少华,郝天姚,等.冲绳海槽及其邻域地球物理场与地壳结构特征[J].地球物理学进展,2003,18(2):287-292.

SHINIJO R,YUZO K.Geochemical constraints on the origin of bimodal magmatism at the Okinawa Trough,an incipient back-arc basin[J].Lithos,2000,54,117-137.

黄朋,李安春,蒋恒毅.冲绳海槽北、中段火山岩地球化学特征及其地质意义[J].岩石学报,2006,22(6):1703-1712.

TERAKADO Y,NAKAMURA N.Nd and Sr isotopic variations in acidic rocks from Japan:significance of upper-mantle heterogeneity[J].Contrib Mineral Petrol,1984,87:407-417.

孟宪伟,杜德文,吴金龙,等.冲绳海槽中段火山岩Sr和Nd同位素地球化学特征及其地质意义[J].中国科学(D辑),1999,29(4):367-371.

NATHAN H D,VAN C K.A model of magmatic crystallization[J].Journal of Petrol,1978,19:66-94.

于增慧,翟世奎,赵广涛.冲绳海槽岩浆包裹体岩石化学成分特征[J].海洋与湖沼,2001,32:474-482.

翟世奎,陈丽蓉,张海启.冲绳海槽的岩浆作用与海底热液活动[M].北京:海洋出版社,2001.

翟世奎,陈丽蓉,申顺喜,等.冲绳海槽早期扩张作用中岩浆活动的演化[J].海洋学报,1994,16(3):61-73.

于增慧,翟世奎,赵广涛.冲绳海槽浮岩中碳、氢同位素组成特征[J].海洋学报,2004,26(6):58-64.

BOTTINGA Y,WEILL D F,Densities of liquid silicate systems calculated from partial molar volumes of oxide components[J].American Journal of Science,1970,269:169-182.

BOTTINGA Y,WEILL D F,RICHET P.Density calculations for silicate liquids:I.Revised method for aluminosilicate composition[J].Geochimica et Cosmochimica Acta,1982,46:909-919.

赵海铃.岩浆物理性质和流体动力学[M].北京:地震出版社,1995.

STOLPER E.The speciation of water in silicate melts[J].Geochimica et Cosmochimica Acta,1982,46:2609-2620.

BOTTINGA Y,WEILL D F.The viscosity of magmatic silicate liquids:a model for calculation[J].American Journal of Science,1972,272:438-475.

URBRAIN G,BAOTTINGA Y,RICHET P.Viscosity of liquid silica silicates and aliumino-silicates[J].Geochimica et Cosmochimica Acta,1982,46:1061-1072.

KUSHIRO I.Changes in viscosity and structure of melts of NaAlSi2O6 composition at high pressures[J].Journal of Geophysical Research,1976,81:6347-6350.

KUSHIRO I.Viscosity,density,and structure of silicate melts at high pressures,and their petrological applications[M]//Physics of Magmatic Processes.Princeton:Princeton University Press,1988.

马昌前.结晶分异作用的岩浆动力学条件[J].地球科学——中国地质大学学报,1989,14(3):245-252.

朱永峰.长英质岩浆中不混溶流体的运移机制[J].地学前缘,1994,1(3/4):119-126.

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