Itacolumite (Flexible Sandstone) From Kaliana, Charkhi Dadri District, Haryana, India

摘要

The objective of this study is to highlight main causes of flexibility in itacolumite from Kaliana Hills, Charkhi Dadri district, Haryana. Results of petrominerological studies, scanning electron microscopy (SEM), 3D analysis of SEM images, and quantitative micro fabric analysis reveal that the intergranular void spaces are significantly higher in more flexible specimen (mean 47.68 mu m) relative to less flexible specimen (mean 14.32 mu m, i.e., <3 times), whereas, non-flexible sandstones show negligible intergranular void spaces (4.97-6.40 mu m). Therefore, it may be envisaged that the flexibility in Kaliana itacolumite is due to the presence of more intergranular void spaces. The chemical corrosion appears to be the main reason for the formation of more void spaces in between the constituent grains in the flexible sandstones. Leaching effect on the grains is evident on scanning electron microscopic (SEM) images. These solution channels and embayment might have removed the significant amount of cementing material and silica by dissolution and solution activity. Thus, obviously, the flexibility in the itacolumite was induced by solution activity, more the solution activity, more the void spaces and hence more resultant flexibility. Almost vertically dipping beds of sandstone would have facilitated capillary movement and solutioning leading to development of concomitant leaching induced porosity.