| 冲绳海槽高热流值区的特征 |
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| 引用本文： | 李常珍,金保生. 冲绳海槽高热流值区的特征[J]. 海洋科学, 1998, 22(5): 50-52 |
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| 作者姓名： | 李常珍 金保生 |
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| 作者单位： | 中国科学院海洋研究所 |
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| 基金项目： | 中国科学院院长基金资助 |
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| 摘 要： | 研究表明，冲绳海槽是一个罕见的高热流值区，是个活动的弧后裂谷，而且热水活动，地震活动，火山活动与之有密切的联系。
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| 关 键 词： | 冲绳海槽 地热流 高热流值区 |
| 收稿时间： | 1998-03-30 |
HIGH HEAT FLOW FEATURES OF THE Okinawa TROUGH |
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| LI Chang zhen JIN Bao sheng. HIGH HEAT FLOW FEATURES OF THE Okinawa TROUGH[J]. Marine Sciences, 1998, 22(5): 50-52 |
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| Authors: | LI Chang zhen JIN Bao sheng |
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| Abstract: | The special geological position of the Okinawa Trough draws the attention of Chinese and foreign scientists. A lot of investigation data indicates that heat flow values of the Okinawa Trough are extremely high. Hydrothermal, eathquake and volcanic activities are very strong, which have a close relation with high heat flow features and indicate that the Okinawa Trough is a very active back arc rift. |
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| Keywords: | Okinawa Trough Heat flow Tectonics |
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