RUI: Fluid Migration Pathways and Fluid Evolution in the Central Appalachians

变形造山带的流体排出是一种 这是一个重要的问题，受到了广泛的关注。 的 这项研究的目的是检查流体流动的中央 阿巴拉契亚前陆褶皱冲断带，决定流体运移 流体成分和温度的变化， 时间 对矿脉中流体包裹体的研究将是今后研究的重点 用于确定区域流体化学平衡的方法 温度和同位素组成。 收集的数据将 纳入前陆水文和热模型。

The expulsion of fluids from deforming orogenic belts is an important subject and has received considerable attention. The purpose of this study is to examine fluid flow in the central Appalachian foreland fold-thrust belt, determine fluid migration pathways and changes in fluid composition and temperature with time. Study of fluid inclusions found in veins will be the primary method used to determine regional fluid chemistry, equilibration temperatures and isotopic composition. Data gathered will be incorporated into foreland hydrologic and thermal models.