流体包裹体面的研究背景、现状及发展前景  

The Background, Application and Development of Fluid Inclusion Planes Research

作　　者：倪培[1] 蒋少涌[1] 凌洪飞[1] 范建国[1] 

机构地区：[1]南京大学地球科学系

出　　处：《地质论评》2001年第4期398-404,共7页Geological Review

基　　金：国家自然科学基金(编号49702023)

摘　　要：在地质流体研究领域,流体包裹体面(Fluid Inclusion Plane——FIP)作为能将地质流体的活动与特定构造和岩浆作用相联系的一种手段,正在发挥越来越重要的作用。并成为流体包裹体研究领域的一个热点。本文对流体包裹体面的研究背景及现状进行了详细的阐述,指出它在地质流体及相关研究领域具有十分广阔的应用前景。More and more attention has been paid to geo-fluid research recently. Fluid inclusion, as the exclusive window for direct observing fluid process, has been proved one of the most powerful means in geo-fluid research field. As definite geological process always result from definite tectonic-hydrothermal event, so it will be undoubtedly very helpful to find a means to link definite geo-fluid process and definite tectonic-magmatic process together. FTP (fluid inclusion planes) is such an effective means. By studying the FIP, we can obtain important information concerning relation of fluid process to rock-forming and ore-forming process. FIP represents the Mode I cracks that occur in sets with predominant orientation perpendicular to the least principal compressive stress axis 3. They are the records of paleofluid now occurring as fluid inclusions in healing cracks of the rock minerals. FIP help us to get a better understanding for rock deformation, regional geological evolution relating to fluid process.

关 键 词：显微构造 流体包裹体面 FIP 地质流体 岩浆作用 形成机制 捕获机制 

分 类 号：P641.2[天文地球—地质矿产勘探]