沉积物热导率是计算海底热流的一个重要参数。
Sediment thermal conductivity is one of the important parameters for computing submarine heat flow.
热流探测是一项重要的基础地球物理调查项目，使用探针式热流计测量海底热流是常用的方法。
The Heat flow probe is the common-used device in measuring seafloor heat flow, which is one of the most important items of geophysical investigations.
利用实测的海底温度和海底热流资料对东海陆坡和冲绳海槽中轴以西的槽底地区的海底温度场和热流场进行了分析。
We analyze the distribution of temperature and heat flow of the sea floor sediment in the area of East China sea slope and West basin area of the Okinawa Trough.
此项工作的成功，将有助于地热流测量工作的深入开展，进而提高我国海底天然气水合物的勘探和海洋地质基础研究的水平。
Its success will be helpful for the further work of Marine geothermal survey and thus improve both the exploration of gas hydrates under the sea and the study of fundamental Marine geology.
此项工作的成功，将有助于地热流测量工作的深入开展，进而提高我国海底天然气水合物的勘探和海洋地质基础研究的水平。
Its success will be helpful for the further work of Marine geothermal survey and thus improve both the exploration of gas hydrates under the sea and the study of fundamental Marine geology.
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