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冲绳海槽海底地形的补偿模式研究Ⅰ.理论均衡响应函数的计算 被引量:6

Study on topographic compensation model of the Okinawa Trough Ⅰ. Calculation of theoretical isostatic response function
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摘要 本文从区域补偿和实验均衡出发,导出了上部负载和下部负载相关时理论均衡响应函数的计算公式,计算了弹性板有效厚度不同以及上部负载和下部负载的比例不同时的理论均衡响应函数曲线,并对曲线形态进行了初步的讨论. ──Based on regional compensation model and experimental isostasy, the isostatic response function of the Okinawa Trough was calculated by using gravity and topographic data. The results are shown as follows: the effective elastic thickness of the plate and compensation depth in the southern Okinawa Trough is obviously greater than those in the middle Okinawa Trough. In reference with other geological and geophysical data, the deferences between the two portions are explained to be caused mainly by their differences in temperature of the lithosphere and the compensation mechanism.
出处 《海洋学报》 CAS CSCD 北大核心 1998年第6期70-75,共6页
关键词 冲绳海槽 地形负载 均衡响应函数 海底地形 The Okinawa Trough, compensation model, isostatic response function, and topographic load, loads from below
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参考文献2

  • 1李乃胜,冲绳海槽地热,1995年,1页
  • 2金性春,海洋地质与第四纪地质,1984年,4卷,3期,17页

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