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墨西哥湾深水下陆坡区冷泉碳酸盐岩中的环烷烃及单环芳烃的特征与来源
管红香1; 陈多福2; 吴能友1
2010
Source Publication海洋地质与第四纪地质
ISSN0256-1492
Volume000Issue:003Pages:113
Abstract研究了墨西哥湾水深约2 200 m的下陆坡Alaminos Canyon 645区块(AC 645区)冷泉碳酸盐岩中含量较高的烷基环戊烷、烷基环己烷、直链烷基苯及苯基烷烃化合物的组成和分布特征。烷基环戊烷和烷基环己烷以低碳数烃占绝对优势,主峰碳分别为C14和C15,目前发现的烷基环己烷主要来源于嗜热嗜酸的细菌或藻类直链脂肪酸经环化作用的产物。烷基苯碳数分布范围为C13—C23,以C13—C20的低碳数烷基苯为主,主峰碳为C16,具有明显偶碳优势,很可能来源于冷泉渗漏环境中的喜盐细菌。
Language英语
Document Type期刊论文
Identifierhttp://ir.giec.ac.cn/handle/344007/20452
Collection中国科学院广州能源研究所
Affiliation1.中国科学院广州能源研究所
2.中国科学院广州地球化学研究所
First Author AffilicationGuangZhou Institute of Energy Conversion,Chinese Academy of Sciences
Recommended Citation
GB/T 7714
管红香,陈多福,吴能友. 墨西哥湾深水下陆坡区冷泉碳酸盐岩中的环烷烃及单环芳烃的特征与来源[J]. 海洋地质与第四纪地质,2010,000(003):113.
APA 管红香,陈多福,&吴能友.(2010).墨西哥湾深水下陆坡区冷泉碳酸盐岩中的环烷烃及单环芳烃的特征与来源.海洋地质与第四纪地质,000(003),113.
MLA 管红香,et al."墨西哥湾深水下陆坡区冷泉碳酸盐岩中的环烷烃及单环芳烃的特征与来源".海洋地质与第四纪地质 000.003(2010):113.
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