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- Generally speaking, we can not see the ocean ridge on the sea. 一般情况下,我们在海面上是看不到海岭的。
- Practical applications for heat flow measurements in ocean floors are the location of hot brines. 洋底热流量测量的实际目的是圈定热卤水的位置。
- The ophiolite partly formed ocean ridge, mainly formed in an ocean island. 蛇绿岩环境分析表明，部分为洋中脊环境，大部分为洋岛环境。
- The geographical distribution of heat flow data is very uneven. 热流量资料的地理分布很不平衡。
- The so-called ocean ridge is a major landforms, and spur its trunk extended to the ocean. 所谓的洋中脊就是一个主要地貌，其主干与支脉延伸至各大洋。
- Steady-state heat flow is comparable to the flow of an incompressible fluid. 稳态热流和不可压缩流体的流动可相比拟。
- Our result shows the nonuniform distribution of mantle heat flow in China. 结果显示;中国大陆地幔热流的空间分布不均匀.
- The mantle flow controls the plate movement and the distribution of ocean ridges, subduction zones, and collision zones. 地幔流动对地表板块运动、海洋中脊和中隆、俯冲带和碰撞带的分布起着控制作用。
- Heat flow from a hotter to a cooler body is a process of energy transfer tending to equalize temperature. 热从高温物体流向低温物体是一个能量传递过程，它使温度趋于均匀。
- The approximation of a linear dependency between heat flow and temperature difference leads to satisfactory results. 在热流量与温度差之间，近似地采用线性关系，也能得出令人满意的结果。
- The rate of heat flow between any two points increases with difference of temperature. 任何两点间的热流动速率则随温差的加大而增加。
- In short, heat flows from the warmer to the cooler body. 总之,热总是从高温物体流向低温物体。
- In heterogeneous anisotropic materials the heat flow vector and conductivity are more complex. 在各向异性的非均质材料中，热流向量和热导率很复杂。
- This type of faulting occurs in response to extension and is often observed in the Western United States Basin and Range Province and along oceanic ridge systems. 这种类型的断层活动是由伸展作用造成的，常常在美国西部的盆岭省以及海底洋岭系统中观测到。
- It is impossible to have a cyclic machine that completely converts the random molecular energy of heat flow into the ordered motion of mechanical work. 不可能得到一种循环机器能把热流的无序的分子能量完全转变为机械功的有序运动。
- For instance the geomagnetic field, the heat flow, the propagation of seismic waves, the force of gravity, etc. 例如，应用地球物理勘探，可以了解诸如地磁场、热流、地震波的传播和重力等地球物理性质。
- The source of heat of the system comes from the heat flow within Tangshan anticline. 该系统以汤山背斜控热构造提供的大地热流为热源；
- Hence peridotite modes can be used to reflect efficiently mantle melting and melt extraction processes beneath ocean ridges only if the excess olivine is removed appropriately. 为此，只要把深海橄榄岩中过量的橄榄石剔除后，其实际矿物组分就能有效地反映洋脊下地幔熔融作用和熔融萃取过程。
- Sediment thermal conductivity is one of the important parameters for computing submarine heat flow. 摘要沉积物热导率是计算海底热流的一个重要参数。
- Indian Ocean ridge seismicity observed with a permanent hydroacoustic network 带有一个永久的水声网络观测的印度海洋脊地震
