GEOFLUIDS

地球流体为研究流体在地壳矿物化学和结构演化中的作用提供了一个国际论坛。它的明确目标是在进行地球流体研究的各个子学科之间传播思想。为此目的，将鼓励作者强调其研究的跨学科相关性，并使来自其他子学科的读者尽可能接近他们的工作。地球流体强调整个地壳地下流体的化学和物理方面(尽管不包括硅酸盐熔体)。地球流体包括地下水、陆地或海底地热流体、盆地卤水、石油变质水或岩浆流体的研究，但需要与在地质时间尺度上具有重要意义的过程相关联。鼓励作者提交描述理论或观测研究的文章，探索地下流体的地质地球化学或地球物理属性，量化对渗透性地球化学输运和热输运的地质控制，或记录地壳流体行为的应用方面。

Geofluids provides an international forum for original research into the role of fluids in mineralogical chemical and structural evolution of the Earth's crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end authors will be encouraged to stress the transdisciplinary relevance of their research and to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes both chemical and physical aspects of subsurface fluids throughout the Earth's crust (although excluding silicate melts). Geofluids spans studies of groundwater terrestrial or submarine geothermal fluids basinal brines petroleum metamorphic waters or magmatic fluids but requires relevance to processes that are significant on a geological time scale. Authors are encouraged to submit articles that describe theoretical or observational studies explore the geologic geochemical or geophysical attributes of subsurface fluids quantify the geologic controls on permeability geochemical transport and heat transport or document applied aspects of crustal fluid behaviour.