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《Geochimica》 1998-03
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ANALYSIS OF ORGANIC INCLUSIONS USING MICRO-FT.IR AND FLUORESCENCE MICROSCOPY AND ITS SIGNIFICANCE

Li Rongxi;Jin Kuili; Liao Yongsheng (Beijing Graduate School, China University of Mining and Technology, Beijing 100083)(Geological Research Institute, Shengli Petroleum Administration, Dongying 257015)  
Organic inclusions from the Shahejie Formation of Eogene Period in Shengli Oil-Gas Province, eastern China were studied using Micro-FT. IR and fluorescence microscopy as well as by measurement of homogenization temperature (Th). Two populations of organic inclusions were recognized, the primary and secondary organic inclusions. The former contains sulfur alcohol and organic materials which have relatively long alkyl chains with the carbon atom number of 15-17, whereas the later contains a certain amount of H2S besides sulfur alcohol, and organic materials have relatively short alkyl chains with the carbon atom number of 5-6. The Th of the primary organic inclusions is 87-91℃ and is lower than that of the secondary inclusions (Th = 98-105℃), suggesting that the primary inclusions experienced a thermal evolution of lower degrees than the secondary inclusions. This inference is consistent with the characteristics of the fluorescence spectroscopy and parameters (λmax,Q values) of the organic inclusions. The composition and thermal maturation of organic inclusions suggest that the primary inclusions resulted from the migrahon of the hydrocarbon-generated organic materials within the stratum where they lived,whereas the secondary organic inclusions are trapped when hydrocarbon migrated secondly out of the source rock to the places where they finally accumulated.
【Fund】: 国家自然科学基金!49672131
【CateGory Index】: P618.13
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