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烃源岩中有机黏粒复合体——天然的生烃母质

蔡进功 宋明水 卢龙飞 包于进 丁飞 徐金鲤

海洋地质与第四纪地质2013,Vol.33Issue(3):123-131,9.
海洋地质与第四纪地质2013,Vol.33Issue(3):123-131,9.DOI:10.3724/SP.J.1140.2013.03123

烃源岩中有机黏粒复合体——天然的生烃母质

ORGANO-CLAY COMPLEXES IN SOURCE ROCKS——A NATURAL MATERIAL FOR HYDROCARBON GENERATION

蔡进功 1宋明水 2卢龙飞 3包于进 2丁飞 1徐金鲤2

作者信息

  • 1. 同济大学海洋地质国家重点实验室,上海200092
  • 2. 中石化胜利油田地质科学研究院,东营257015
  • 3. 中石化石油勘探开发研究院无锡石油地质研究所,无锡214151
  • 折叠

摘要

Abstract

Traditionally,it is believed that kerogen,a organic matter insoluble in organic solvents separated chemically from source rock,is a material for hydrocarbon generation[1].The procedure to treat samples as such,however,may destroy the original occurrence and relationship between organic matter and clay in source rocks.We extracted an organo-clay complex (<2μm) from the crushed source rocks in the depth of 280~3 500 m,in the Jiyang sag,East China.The complex is mainly composed of layered illite-smectite ((Ⅰ)-S) and illite with a value of TOC up to 2.62%~9.78%.After treatment with H2O2.TOC remains as high as 1.23%~4.63%,suggesting that it is the components in which organic matters are enriched.The diffraction peak (d001) of the complex is 1.3~1.4nm at 250℃,and moves to 1.0 nm at 550 ℃ in XRD curves,and the exothermic peaks of the complex is extraordinary stable at 350 ℃ in DTA curves.; The result is consistent in both the XRD and DTA observations.It indicates that organic matter can enter the interlayer space of clay minerals.With PY-GC analysis,the organic matter of C5 and C25 is released from the complex in a temperature range of 250~650 ℃,and reaches a peak at about 450 ℃.Our findings reveal that organic matter can enter interlayer of clay minerals forming a kind of natural and highly stable organo-clay complex,and the composition of the organic matter in the complex is similar to the crude oil.As a kind of natural material,the organo-clay complex plays an important role in hydrocarbon generation in source rocks.

关键词

有机黏粒复合体/有机质富集/特性稳定/天然生烃母质

Key words

organo-clay complexes/ organic enrichment/ property stability/ hydrocarbon generation material

分类

天文与地球科学

引用本文复制引用

蔡进功,宋明水,卢龙飞,包于进,丁飞,徐金鲤..烃源岩中有机黏粒复合体——天然的生烃母质[J].海洋地质与第四纪地质,2013,33(3):123-131,9.

基金项目

国家自然科学基金项目(41072089) (41072089)

国家油气重大专项(2011ZX05006-001) (2011ZX05006-001)

中国石油化工有限公司科技局基金项目(P11039) (P11039)

海洋地质与第四纪地质

OA北大核心CSCDCSTPCD

0256-1492

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