Experimental evidence that fluid inclusions do not leak
Experimental evidence that fluid inclusions do not leak
复制标题
流体包裹体不会泄漏的实验证据
DOI：
10.2113/gsecongeo.63.7.715
复制
发表时间：
1968
期刊：
影响因子：
--
通讯作者：
B. Skinner
中科院分区：
文献类型：
--
作者：
E. Roedder;B. Skinner
新的实验是在小的石英晶体和闪锌矿和方解石的解理碎片上进行的，不需要锯、磨或抛光。石英样品在2000巴和4000巴的外部水压和100摄氏度至400摄氏度的温度下运行长达17天。在某些运行中，内部压力超过外部2000-3000巴。“从这项工作和文献回顾中，[作者]得出结论，大多数内含物没有遭受重大泄漏。之前的一些实验表明泄漏可以通过样品制备过程中引入的微裂缝来解释。“泄漏，通过扩散，像氢这样的物质不排除。
New experiments were performed on small quartz crystals and cleavage fragments of sphalerite and calcite, none requiring sawing, grinding or polishing. Quartz samples were run at external water pressures of 2000 and 4000 bars, and temperatures from 100 degrees to 400 degrees C for up to 17 days. Internal pressures exceeded external by 2000-3000 bars in some runs. 'From this work and a review of the literature [authors] conclude that most inclusions have not suffered major leakage. Some previous experiments indicating leakage may be explained by microfractures introduced during sample preparation.' Leakage, by diffusion, of substances like hydrogen is not precluded.