△C的影响因素及其修正的探讨 |
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引用本文: | 李庆军.△C的影响因素及其修正的探讨[J].石油实验地质,1993,15(2):220-224. |
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作者姓名: | 李庆军 |
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作者单位: | 地质矿产部华北石油地质大队, 郑州 450006 |
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摘 要: | △C理论认为,只有油气成因的蚀变碳酸盐在500~600℃温度下产生热分解.作者通过实验认为,其它成因的次生碳酸盐也可在500~600℃下大量分解.换句话说,这些次生的非晶质的碳酸盐(包括△C)可能是该温区分解的主要物质.鉴此,作者根据它们之间函数关系,对其测值进行修正.
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关 键 词: | 非晶质 次生碳酸盐 △C影响因素 |
收稿时间: | 1990-12-29 |
APPROACH THE INFLUENTIAL FACTOR △C AND ITS MODIFICATION |
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Affiliation: | North China Research Party of Petroleum Geology, MGMR |
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Abstract: | With △C theory,it is believed that a pyrolysis will take place only in the altered carbonate of hydrocarbon generation under the temperature range of 500~600℃.However,through the experiments,the author concludes that much pyrolyses will occur in the secondary carbonates of other origins at the temperatures of 500~600℃.It means that these secondary noncrystalline carbonates( including △C)are the major pyrolytic products within the temperature range.In view of this,the author modifies their measurements based on the functional relationships between the carbonates. |
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