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琉球沟弧盆系的海底热流分布特征及冲绳海槽热演化的数值模拟
引用本文:栾锡武.琉球沟弧盆系的海底热流分布特征及冲绳海槽热演化的数值模拟[J].海洋与湖沼,1997,28(1):44-48.
作者姓名:栾锡武
作者单位:中国科学院海洋研究所!青岛,266071
基金项目:国家自然科学基金!49376266
摘    要:以1993-1995年对琉球沟弧盆系各个航次的热流数值进行了搜集整理,发现这一地区热流的分布特征和构造特征有明显的对应关系,大致上呈出现东西分带南北分块的分布特征,冲绳海槽有极高的热流值,而琉球海沟则有极低的热流值,这和板块的撞碰,俯冲,弧后扩张模式相吻合,用二维热传导平流议程用有限单元法对冲绳海槽进行的地球动力学热模拟显示,冲绳海槽的高热流值和海槽内的岩浆活动有着密切关系,如果不考虑海槽中岩浆因

关 键 词:琉球沟弧盆系  热流分布  海底  数值模拟  冲绳海槽
收稿时间:1995/3/21 0:00:00
修稿时间:1996/5/29 0:00:00

STUDY OF HEATFLOW DISTRIBUTION OF RYUKYU TA-B-A SYSTEM AND THERMO DYNAMIC MODELING OF OKINAWA TROUGH
Luan Xiwu.STUDY OF HEATFLOW DISTRIBUTION OF RYUKYU TA-B-A SYSTEM AND THERMO DYNAMIC MODELING OF OKINAWA TROUGH[J].Oceanologia Et Limnologia Sinica,1997,28(1):44-48.
Authors:Luan Xiwu
Institution:Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071
Abstract:Review of 320 data sets of heatflow data measured in 1993-1995 during 15 cruises in the Ryukyu TA-B-A system showed that the hestflow in the deep, trench region was sub -normal; that trench -arc gaps were generally characterized by lower heattflow agreeing with the prediction from plate -cooling models the Okinawa Trough, an actively spreading back arc basin had highly variable heatflow indicating modern volcanism and hydro-thermal circulation in the new crust. The distribution of heatflow agreed with the tectonic pattern of the Ryukyu TA-B-A system, 2-D nonsteady -state heat advective-conduction equations were used to simulate tectonically thermal evolution in this study showing that the effects of magnatic activity in the Okinawa Trough region are important to, and can explain, the observed high surface heatflow. A flow function used to describe the mantle flow under the Okinawa Trough shows that the crustal thickness in the region is about 18tri; that the Trough extension rate is O.4cm /a; that the surface subsidence rate is O.O5cm /a; and that the thermal process of the Trough is about 1O mi1lion years.
Keywords:Ryukyu  TA-B-A system  Heatflow distribution  Thermo evolution  Modeling  
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