Areas in which andesitic volcanic rocks have been formed by volcanic activity in a submarine environment are distributed from Hokkaido to southwestern Japan (Sanin Province) along the Sea of Japan (so-called green tuff region). Rock collapses and tunnel deformations often occur in these areas. The mode of occurrence, characteristics of smectite, pore-size distribution and slaking properties of andesitic volcanic rocks distributed in the middle part of Akita Prefecture were studied to clarify the causes of rock collapses and tunnel deformations.
In the rocks that show strong slaking properties, the distance between plagioclase crystals is large and the interstices between the crystals are filled with smectite. The rocks also contain large amounts of pores having diameters from 500 nm to about 10,000 nm. The rocks having the characteristics presented above are rocks consisting of the rim of a pillow lobe, matrix of pyroclastic rocks and volcaniclastic rocks having textures in which boundaries between the fragments and matrix are obscure. It is thought that slaking properties of andesitic volcanic rocks formed by submarine volcanic activity are controlled by the quantity of smectite, style of distribution of minerals (distance between plagioclase crystals) and pore distribution. Focusing on the mode of occurrence and physical properties of diagenetically altered andesitic volcanic rocks formed in a submarine environment is important for preventing disasters from the point of view of applied geology.
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