| 内蒙古海拉尔盆地侏罗系烃源岩地球化学特征 |
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| 引用本文： | 李娇娜,徐然,张健,朱焕来,申家年.内蒙古海拉尔盆地侏罗系烃源岩地球化学特征[J].地质与资源,2017,26(2):147-156. |
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| 作者姓名： | 李娇娜 徐然 张健 朱焕来 申家年 |
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| 作者单位： | 1. 东北石油大学 地球科学学院, 黑龙江 大庆 163318;2. 中国地质调查局 沈阳地质调查中心(沈阳地质调查矿产研究所), 辽宁 沈阳 110034 |
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| 基金项目： | 中国地质调查局研究专项“海拉尔和二连盆地侏罗系烃源岩特征研究” |
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| 摘 要： | 在海拉尔盆地外围及周边地区选取了31块侏罗系野外烃源岩分析样品，进行了总有机碳、岩石中可溶有机质的抽提和岩石热解分析；针对该区侏罗系烃源岩，共对17口井岩心进行了取样地化分析，利用气相色谱-质谱对烃源岩氯仿抽提物及重要生物标志化合物开展了定性与定量检测，目的是对源岩地球化学特征进行系统评价，为下一步油气基础地质调查奠定基础.结果表明，海拉尔盆地外围及周边地区的侏罗系部分的烃源岩有机质丰度较高，应具备较好的生烃物质基础.海拉尔盆地侏罗系烃源岩总体属于淡水-半咸水环境，有机质类型多样，成熟度普遍较高.甾类化合物中以规则甾烷为主，沉积物中具有较高丰度的以五环三萜烷为主的三环萜烷化合物，显示了其应以藻类生源为主，高等植物为主的陆相沉积中的相对含量则较低.伽马蜡烷的含量普遍很低.OEP呈偶碳数优势，并且缺失高分子正构烷烃，说明烃源岩成熟度演化早期受到了微生物降解作用.
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| 关 键 词： | 海拉尔盆地 侏罗系 地球化学 生物标志化合物 内蒙古 |
| 收稿时间： | 2016-07-13 |
GEOCHEMISTRY OF THE JURASSIC SOURCE ROCKS IN HAILAR BASIN,INNER MONGOLIA |
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| LI Jiao-na,XU Ran,ZHANG Jian,ZHU Huan-lai,SHEN Jia-nian.GEOCHEMISTRY OF THE JURASSIC SOURCE ROCKS IN HAILAR BASIN,INNER MONGOLIA[J].Geology and Resources,2017,26(2):147-156. |
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| Authors: | LI Jiao-na XU Ran ZHANG Jian ZHU Huan-lai SHEN Jia-nian |
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| Institution: | 1. College of Earth Sciences, Northeast Petroleum University, Daqing 163318, Heilongjiang Province, China;2. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China |
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| Abstract: | In the periphery and surrounding areas of the Hailar Basin,31 samples of Jurassic source rocks from the field are selected to analyze rock pyrolysis,extraction of soluble organic matter from rocks and total organic carbon.In order to study the Jurassic hydrocarbon source rocks in this area,cores from 17 wells are sampled and analyzed.The chloroform extracts of the hydrocarbon source rocks and significant biomarkers are detected qualitatively and quantitatively with gas chromatography-mass spectrometry,aiming to systematically evaluate the geochemical characteristics of the source rocks for further geological survey of oil and gas.The results show that the source rocks in the periphery and surrounding areas of Hailar Basin are of high organic matter abundance,with good hydrocarbon generating condition.The environment of the Jurassic source rocks in Hailar Basin belongs to fresh water-brackish water,with diverse types of organic matter and generally high maturity.The steroids are of mainly regular sterane type.The sediment contains high abundance of tricyclic terpane,mainly as pentacyclic triterpane,reflecting a high content of algae.The content of gammacerane is very low.The advantage of even carbon number of OEP and the absence of high molecular normal paraffin shows that the maturity of hydrocarbon source rock has been degraded by microorganisms in the early stage. |
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| Keywords: | Hailar Basin Jurassic geochemistry biomarker Inner Mongolia |
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