氨基酸、脂肪酸对过渡带气、低熟原油形成的意义

对草海盆地泥炭、柴窝堡盆地第四系沉积物以及辽河东部凹陷、胜利东营凹陷、苏北金湖凹陷等第三系烃源岩中氨基酸、脂肪酸进行定性、定量分析，并开展热模拟实验。研究表明氨基酸主要赋存于沥青中，分解后可以生成烃类气体和Ｎ_２气，对过渡带气的形成可作出贡献。烃源岩干酪根和沥青中的脂肪酸含量不少，沥青中脂肪酸以一元酸为主，具偶碳优势，干酪根中脂肪酸以二元酸为主，不具偶碳优势。沥青和干酪根中脂肪酸脱羧基后产生烷烃，对过渡带气和低熟油都可作出贡献，沥青中脂肪酸是生成低熟油中具奇碳优势正烷烃的主要物源。

Significance of Amino Acids and Fatty Acids for the Formation of the Bio-thermocatalytic Transition Zone Gases

The amino acids and fatty acids in sediments of Caohai, Chaiwopu, Liaohe, Jiyang and Subei Basins were quantitatively analysed in this study. Based on the results, the gas-generating tests of peat and mudstone were carried out to investigate distribution and compostition of fatty acids in the extract and kerogen. As a result, some points are drawn as follows:1. Amino acids in sediments are mainly present in the soluble organic matter and may produce hydrocarbons during early diagenesis stage,contributing to the formation of Bio - thermocatalytic Transition Zone Gases.2.α-fatty acids in sediments are mainly present in asphaltene and may produce hydrocarbon, contributing to the formation of immature oil during early diagenesis stage.3. Kerogen is rich in α,ω - fatty acids which are favourable to the generation of Bio-thermocatalytic Transition Gases during erly diagenesis stage, and produce hydrocarbon in mature oil druing oil generating stage.