地史时期“泥裂”构造的成因初探
ORIGIN OF “MUD CRACK” IN THE GEOLOGIC PAST
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摘要: 在今天的自然界,我们常常可以在河漫滩、湖边或者海边看到泥裂,这种泥裂构造是未固结的沉积物露出水面,受到太阳曝晒或者沉积物自然脱水而干涸时发生收缩和裂开所形成的裂隙。它常见于粘土质、粉砂质以及泥灰质沉积物中,其形态在平面上呈网格状,常把沉积物切成边缘向上翘起的多角形块状;在断面上呈“V”形,有时呈“U”字形裂隙常为上覆较粗的沉积物所充填,而且多为单层沉积,很少成为连续的稳定的多层广泛Abstract: Mud crack is a general term used to describe a fissure that forms in finegrained soils and sediments as voiume is reduced during dewatering.The presencc of the crack structure in mudstone and limestone is usually considered by many geologists in China as evidence of an air-drying during a period of surface exposure and is often called sun crack or mud crack. The current study shows,however, that crack formed in the geologic past might be usually generated in argillaceous deposits during a period of uninterrupted water cover by increasing the salinity of the aqueous milieu (the salt concentration was not very high). So this crack should be termed subaqucous syneresis crack or subaqueous shrinkage crack.The term mud or sun crack is sometimes used interchangeably with syneresis crack,but is misleading.