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基性熔体的下垫作用是地壳生长的一种重要方式,并且代表了一种有效的幔向壳的物质与能量迁移。
Underplating of basic melt beneath the crust is one of the most important patterns of crust growth and represents an effective material and energy transfer from the mantle to the crust.
常压下页岩与水基泥浆之间的物质迁移中主要以流动和扩散方式进行。
The main patterns of substance transport between shale and water based mud under low pressure are flow and diffusion.
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