| 东营凹陷沙三段烃源岩中火成岩岩石学特征分析 |
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| 引用本文： | 翟庆龙,张允建.东营凹陷沙三段烃源岩中火成岩岩石学特征分析[J].矿物岩石,2003,23(1):25-29. |
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| 作者姓名： | 翟庆龙 张允建 |
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| 作者单位： | 1. 中国石化胜利油田股份公司,山东,东营,257015;中国科学院地球化学研究所,贵州,贵阳,550002
2. 中国石化胜利油田股份公司,山东,东营,257015 |
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| 基金项目： | 石油企业中青年创新基金，石油大学 2 11科研基金 (EX-99-0 9) |
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| 摘 要： | 东营凹陷沙三段烃源岩中发现一些规模不大的玄武岩和辉长岩体。通过对其岩性及产状、岩石化学和地球化学元素分析，认为研究区玄武岩是碱性－亚碱性橄榄玄武岩；辉长岩的岩石化学和微量元素组成与上述玄武岩相似，认为它们具有同源性，只是辉长岩没有喷发到地表而被封存在刚刚沉积下来的沙三段烃源岩中。水下喷溢的玄赋岩对烃源岩的沉积和生烃演化具有促进作用，辉长岩可以造成局部烃源岩的热变质作用。
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| 关 键 词： | 火成岩 岩石化学 微量元素 烃源岩 东营凹陷 |
| 文章编号： | 1001-6872(2003)01-0025-05 |
| 修稿时间： | 2002年8月10日 |
INVESTIGATION ON LITHOLOGY OF THE IGNEOUS ROCKS IN THE HYDROCARBON SOURCE ROCKS IN THE THIRD MEMBER OF THE SHAHEJIE FORMATION,DONGYING DEPRESSION |
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| ZHAI Qing long l,ZHANG Yun jian.INVESTIGATION ON LITHOLOGY OF THE IGNEOUS ROCKS IN THE HYDROCARBON SOURCE ROCKS IN THE THIRD MEMBER OF THE SHAHEJIE FORMATION,DONGYING DEPRESSION[J].Journal of Mineralogy and Petrology,2003,23(1):25-29. |
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| Authors: | ZHAI Qing long l ZHANG Yun jian |
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| Institution: | ZHAI Qing long l,2,ZHANG Yun jian 1 1.The Shengli Oil Com.Lid,Sinopec,Dongying 257015,China, 2.Open Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Science,Guiyang 550002,China |
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| Abstract: | Igneous rocks of basalt and gabbro have been discovered within the hydrocarbon source rocks in the Third Member of the Shahejie Formation in the Dongying depression.Research on the 1ithology, textures, chemical composition and trace elements of the basalt and gabbro showed that the basalts are exactly alkali or sub alkali olivinebasalts.Chemical compostions and trace elements of the gabbro are derived similar to those of the basalts, so the gabbro and basalt are considered to have the same genetic source derived from the mantle.The gabbro intruded into the source rocks,instead of going up and flowing out on the surface. |
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| Keywords: | igneous rock rock chemical composition trace element hydrocarbon source rock Dongying depression |
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