| 鄂尔多斯盆地北缘固阳县北中元古界长城系烃源岩地质特征及意义 |
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| 引用本文： | 冯娟萍 欧阳征健 范萌萌. 鄂尔多斯盆地北缘固阳县北中元古界长城系烃源岩地质特征及意义[J]. 地质科学, 2020, 55(4): 1044-1055. doi: 10.12017/dzkx.2020.064 |
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| 作者姓名： | 冯娟萍 欧阳征健 范萌萌 |
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| 作者单位： | 西安科技大学地质与环境学院 西安 710054 煤炭绿色开采地质研究所 西安 710054 兰州城市学院培黎石油工程学院 兰州 730070 |
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| 基金项目： | 国家自然科学基金青年项目（编号：41502107）资助； |
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| 摘 要： | 是否发育有效烃源岩是鄂尔多斯地区中元古界成藏的关键。综合利用野外地质考察、显微薄片鉴定和地球化学分析等研究方法对固阳县北中元古界渣尔泰山群阿古鲁沟组烃源岩地质特征开展研究。研究表明，中元古界烃源岩岩性为低级区域变质作用形成的炭质板岩及片岩，其矿物成分以石英为主，其次为斜长石、钾长石及白云母，还有少量菱铁矿。烃源岩有机碳含量高，变化在0.17%～21.62%之间，平均值为5.53%；有机质类型以Ⅰ型为主，其次为Ⅱ型；Ro变化范围为4.32%～5.09%，Tmax值介于556 ℃～564 ℃，处于过成熟阶段。稀土元素体现出LREE富集和轻、重稀土分异明显的特点，δEu介于0.43～0.49之间，表现出Eu的明显负异常；微量元素含量及比值指示阿古鲁沟组烃源岩形成时的沉积环境为水体深度大、水动力条件弱的并且与外海沟通受到限制的贫氧—缺氧的闭塞环境，沉积相类型为温暖潮湿气候条件下淡化泻湖相。
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| 关 键 词： | 固阳县北 中元古界 烃源岩 地质特征 地球化学 |
| 收稿时间： | 2020-03-30 |
| 修稿时间： | 2020-05-30 |
Geological characteristics and significance of source rocks of Mesoproterozoic Changchengian System in north of Guyang County of the northern margin of Ordos Basin |
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| Feng Juanping Ouyang Zhengjian Fan Mengmeng. Geological characteristics and significance of source rocks of Mesoproterozoic Changchengian System in north of Guyang County of the northern margin of Ordos Basin[J]. Chinese Journal of Geology, 2020, 55(4): 1044-1055. doi: 10.12017/dzkx.2020.064 |
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| Authors: | Feng Juanping Ouyang Zhengjian Fan Mengmeng |
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| Affiliation: | College of Geology and Environment, Xi´an University of Science and Technology, Xi´an 710054 Geological Research Iinstitute for Coal Green Mining, Xi´an 710054 Bailie School of Petroleum Engineering, Lanzhou City University, Lanzhou 730070 |
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| Abstract: | The development of effective source rocks is the key to Mesoproterozoic hydrocarbonaccumulation in Ordos area. In this paper, the geological characteristics of source rocks in theAgulugou Formation of the Zhaertaishan Group of Mesoproterozoic Changchengian System in northof Guyang County were studied by means of field geological investigation, microscopic sectionidentification and geochemical analysis. Researches show that the source rock is carbonaceous slateand a small amount of schist with quartz as the main mineral composition, followed by plagioclase, potassium feldspar and muscovite, and a small amount of siderite. The contents of organic carbonin the source rocks are high, and the value ranges from 0.17% to 21.62%, with an average of 5.53%.The type of organic matter is Ⅰ kerogen, and the second is Ⅱ kerogen. The value of Ro ranges from 4.32% to 5.09%, and the Tmax value is from 556 ℃ to 564 ℃. These results show that the thermal evolution of source rocks is high, and is in the over-mature stage. Their NASC normalized REE patterns of the source rocks are characterized by LREE enrichment with obvious different valuebetween LREE and HREE with distinctive negative Eu anomalies（δEu: 0.43～0.49）. The content and ratio of trace elements indicate that the sedimentary environment of the source rocks of Agulugou Formation is an oxygen-deficient-anoxic closed environment with large water depth, weakhydrodynamic conditions and limited communication with the open sea and the sedimentary faciesare desalinated lagoon facies in warm and humid climate. |
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