东营凹陷沙河街组砂岩中自生高岭石特征及其成因探讨*

南京大学学报(自然科学版) ›› 2013, Vol. 49 ›› Issue (3): 331–342.

东营凹陷沙河街组砂岩中自生高岭石特征及其成因探讨*

张雪芬1，陆现彩1**，刘庆2，张林哗2，李娟1，马野牧1，张立虎1

出版日期:2015-11-13 发布日期:2015-11-13
作者简介: (1.内生金属成矿机制国家重点实验室，南京大学地球科学与工程学院，南京，210093;
2.中石化胜利油田分公司地质科学研究院，东营，257015)
基金资助:
国家自然科学基金(40973029,41072096)

Characteristics and genetic mechanism of authigenic kaolinite in the
sandstones of the Shahejie formation in the Dongying depression

Zhang Xue- Fen¹ ,Lu Xian-Cai¹ ,Zhang Lin-Ye² ,Liu Qing² ,Li Juan¹
Ma Ye-Mu¹，Zhang Li -Hu¹

Online:2015-11-13 Published:2015-11-13
About author: (1 .State Key Laboratory for Mineral Deposits Rescarch,School of Earth Sciences and Engineering,
Nanjing University,Nanjing,210093,China;
2. Geological Science Research institute of Shengli Oilficld,Dongying,257015,China)

摘要/Abstract

摘要： 东营凹陷沙河街组砂岩是胜利油区主要的储集层，自生高岭石是该储层中最常见的自生粘
上.通过显微镜和扫描电镜观察，并结合X射线衍射和电子探针成分分析，发现碎屑粘上含量极少，自生
高岭石为主，其集合体呈书页状和蠕虫状，长石碎屑的溶蚀现象多见;高岭石多充填在次生孔隙内，原生
孔隙中亦可见.通过分析碳酸盐胶结物的碳氧同位素组成研究了砂岩成岩流体与烃源岩间的可能继承
关系，自生高岭石的形成主要受烃源岩成岩演化过程中排出的含烃流体影响，推测酸性的含烃流体与长
石的相互作用是高岭石形成的主要机制.统计表明:高岭石的含量与岩石的孔隙度表现出较好的正相关
性，亦支持其形成于长石溶蚀的观点.

Abstract: The sandstones of the Shahejie formation in the Dongying depression are the mam reservoms in Shengli
(Oil Field. Kaolinite is the most common authigenic mineral in these reservoirs. By employing multiple techniques in-
cluding scanning electron microscopy(SEM)，X-ray diffraction(XRD)and electron probe micro-analyzer(EPMA),it is
confirmed that little elastic clays exist in sandstones while large amount of authigenic kaolinitc have precipitated.The
kaolinite occurs as agglomerates of booklets or vermicular crystals，which generally fill in secondary pores from dis-
solution of feldspars as well as in primary pores. Carbon and oxygen isotopes of carbonate cements were analyzed in
order to better understand the inheritance relationship between diagenesis fluids of sandstones and source rocks.The
results indicate that the fluid released from source rocks accompanying with hydrocarbon generation can result in the
dissolution of elastic feldspar and the formation of authigenic kaolinite. So it is considered that the interaction of acid-
ic hydrocarbon bearing fluid with feldspars is the primary genetic mechanism of anthigenic kaolinites.Statistics anal
ysis shows that the content of kaolinites is well correlated to porosity in reservoirs, and anthigenic kaolinitcs are
closely related to the dissolution of feldspars.

张雪芬1，陆现彩1**，刘庆2，张林哗2，李娟1，马野牧1，张立虎1
. 东营凹陷沙河街组砂岩中自生高岭石特征及其成因探讨*[J]. 南京大学学报(自然科学版), 2013, 49(3): 331–342.

Zhang Xue- Fen¹ ,Lu Xian-Cai¹ ,Zhang Lin-Ye² ,Liu Qing² ,Li Juan¹
Ma Ye-Mu¹，Zhang Li -Hu¹. Characteristics and genetic mechanism of authigenic kaolinite in the
sandstones of the Shahejie formation in the Dongying depression
[J]. Journal of Nanjing University(Natural Sciences), 2013, 49(3): 331–342.

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