由于对前高加索东部第三纪和中生代地层中粘土矿物和其组合的分布特征进行了研究,作者得出结论,蒙脱石水云母化是分散有机物向生油方向转化的判别标志之一。水云母化的过程伴随着能量的放出,而这能量可利用来为有机物进一步的转化。由于水云母吸附能力比蒙脱石小,因此水云母化将促使已变化的有机化合物的迁移。 Due to the distribution characteristics of clay minerals and their assemblages in the Tertiary and Mesozoic strata in the eastern Caucasus, the authors concluded that the montmorillonite hydration is one of the distinguishing criteria for the diversion of organic matter into the oil. Water michemization is accompanied by the release of energy, which can be exploited to further transform organic matter. Because mica has less adsorption capacity than montmorillonite, hydration will promote the migration of the already-changing organic compounds.