Scales and Effects of Fluid Flow in the Upper Crust
Scales and Effects of Fluid Flow in the Upper Crust
复制标题
上地壳流体流动的规模和影响
DOI：
10.1126/science.248.4953.323
复制
发表时间：
1990
期刊：
影响因子：
56.9
通讯作者：
L. Cathles
中科院分区：
文献类型：
--
作者：
L. Cathles
地质变化的两个最重要的因素，太阳能和来自地幔的内部热量，相遇并争夺主导地位，推动地球上地壳中的水和相关流体。哪一种占主导地位以及它们如何相互作用是积极研究的主题。最近的研究表明，这两种介质都可以推动流体在近大陆尺度的距离上运动，影响许多重要的地质过程，并在化学蚀变、矿床和碳氢化合物资源中留下记录。
Two of the most important agents of geological change, solar energy and internal heat from the mantle, meet and battle for dominance in propelling aqueous and related fluids in the earth's upper crust. Which prevails and how they interact are subjects of active research. Recent work has demonstrated that both agents can propel fluids over nearly continental-scale distances in a fashion that influences a host of important geological processes and leaves a record in chemical alteration, mineral deposits, and hydrocarbon resources.