含油气盆地naftides微量元素研究

S. Punanova, С А Пунанова
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引用次数: 0

摘要

研究了世界各油气盆地油田中微量元素的浓度分布参数、理化性质以及盆地成油的地质地球化学特征。研究表明,深部构造作用(地球动力因素)对烃类的成因不仅控制着烃类在沉积盖层中的位置,而且还控制着其成矿专一性的多样性。根据矿质元素的富集程度和属钒或镍成矿类型,对不同成因带的油进行了分类。呈现出主要成油带初始富微量元素和早期成油带初始低微量元素的特征。在深生带,油的组成变化导致其富集,而在变质带,油的微量元素被耗尽。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Trace elements of naftides of oil- and gas-bearing basin
The parameters of the concentration distribution of trace elements in the oil fields of oil and gas basins of the world, their physic-chemical properties, as well as the geological and geochemical features of oil formation in these basins were studied. It is shown that the ontogenesis of hydrocarbons associated with deep tectonic transformations (geodynamic factor) controls not only the placement of naphtides in the sedimentary cover, but also the diversity of their metallogenic specialization. The classification of oils of various ontogenesis zones is given in accordance to the degree of their enrichment of mineral elements and their belonging to the vanadium or nickel metallogenic type. The oil, characterized by primary rich concentrations of trace elements of the main zone of oil formation, and oil with initially low concentrations of trace elements in the zones of early generation are presented. The processes of transformation of the composition of oils in the areas of hypergenesis lead to their enrichment, whereas the oil of the catagenesis zone is depleted in trace elements.
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