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本文对深海钻孔资料(360处)的综合性系统的分析结果以及笔者亲自进行的“全球大洋沉积层中自生沸石的分布及相位置研究”进行了论述。笔者对全新世、更新世、中新世始新世和白垩纪所编的沸石分布示意图证实了前人的沸石全球性分层的看法。该图表明,钙十字沸石主要形成于全新世一中新世,而斜发沸石主要形成于始新世和白垩纪,这两种沸石在渐新世和中新世都有广泛分布。钙十字沸石与斜发沸石的相位置,矿物的共生组合,以及它们的物质来源都不相同。大洋中沸石全球性垂直分层很可能是那时火山作用性质的变化以及全球大洋沉积物普遍演化引起的。
This paper analyzes the comprehensive system analysis of deep-sea borehole data (360 sites) and the author’s own study on the distribution and phase location of the zeolite in the global oceanic sediments. The author’s illustrations of the zeolite distributions for the Holocene, Pleistocene, Miocene and Cretaceous confirm the global stratification of the previous zeolites. The figure shows that Ca-Phillipsite was predominantly formed during the Holocene-Miocene, whereas clinoptilolite was mainly formed in the Eocene and Cretaceous, both of which are widely distributed in Oligocene and Miocene. The phase location of calcium phillipsite and clinoptilolite, the symbiotic combination of minerals, and their material sources are not the same. The global vertical stratification of zeolites in the ocean is most likely due to the volcanic nature of the volcano at that time and to the general evolution of global ocean sediments.