盆地中热流体-岩石相互作用研究概述  

Research Advance of the Interaction between Hot Fluid Flow and Rocks

作　　者：聂逢君[1] 夏菲[1] 姜美珠[1] 

机构地区：[1]东华理工大学,江西抚州344000

出　　处：《东华理工学院学报》2007年第2期137-143,共7页Journal of East China Institute of Technology

基　　金：国家自然科学基金(40376043)

摘　　要：热流体与岩石的相互作用已经成为了当今地学界研究和关注的热点。它的研究方法和手段的日臻成熟,使得研究内容不断丰富,研究成果推陈出新。总结和概括了国内外流体(热流体),及其与岩石的相互作用的研究现状与成果,尤其是含油气盆地中热流体与砂岩的相互作用后,岩石孔隙度和渗透性、热流体作用的各种标志等作了全面的概述,期望对从事该领域的研究者有一定的借鉴。Research on the interaction between hot fluid flow and rocks has aroused great enthusiasm of geoscientists. The achievements in this field are attributable to a various of analytical methods, such as fluid inclusion, isotopes of element 0 and C, probe, and cathode luminescence etc. This paper displays the update research advances in the interaction between fluid flow and rocks, especially the interaction between hot fluid flow and sandstones in the oil-bearing basins. The current discernible markers left by the interaction are integrated and the porosity and permeability variation with intensity of the interaction are generalized in this paper. All these generalizations are hoped to help the future researchers in this field.

关 键 词：热流体 岩石 相互作用 

分 类 号：P618.130.2[天文地球—矿床学]