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| 渤海湾盆地石炭-二叠系微量元素特征及其指相意义 | |
| 引用本文： | 苗耀,桑树勋,林会喜,陈世悦,李军,杨勇.渤海湾盆地石炭-二叠系微量元素特征及其指相意义[J].沉积与特提斯地质,2007,27(4):27-32. |
| 作者姓名： | 苗耀 桑树勋 林会喜 陈世悦 李军 杨勇 |
| 作者单位： | 1. 中国矿业大学,资源与地球科学学院,江苏,徐州,221008 2. 胜利油田有限公司,地质科学研究院,山东,东营,257015 3. 中国石油大学,地球与信息科学学院,山东,东营,257000 |
| 基金项目： | 国家重点基础研究发展计划(973计划);国家油气专项基金 |
| 摘 要： | 本文采用ICP-MS测试分析技术,对渤海湾盆地4口钻井42件石炭—二叠系岩心样进行了Sr、Ba、Ga、V、Ni、Co等沉积环境敏感元素的系统测试分析,讨论6种元素含量及Sr/Ba、Ba/Ga、Ni/Co等比值的变化特征。除去5件样品中的异常点,测试元素大多数集中的变化范围:Sr(100~200)×10-6,Ba(100~700)×10-6,Ga(10~40)×10-6,V(80~200)×10-6,Co(5~30)×10-6,Ni(15~45)×10-6,Sr/Ba 0.2~0.9,Ba/Ga 2~20,Ni/Co 1~4。根据微量元素指标特点结合岩相资料,认为渤海湾盆地本溪组发育海相沉积,太原组发育过渡相沉积,山西组及其以上地层发育陆相沉积。元素指标中,Ba、Sr/Ba和Ba/Ga沉积环境指示意义显著,在判断渤海湾盆地石炭—二叠纪沉积相方面具有实用价值。 |
| 关 键 词： | 渤海湾盆地 石炭-二叠系 微量元素 沉积相 |
| 文章编号： | 1009-3850（2007）04-0027-06 |
| 收稿时间： | 2006-11-05 |
| 修稿时间： | 2007-03-19 |
Trace element signatures of the Carboniferous -Permian deposits in the Bohai Gulf Basin and their facies significance |
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| MIAO Yao,SANG Shu-xun,LIN Hui-xi,CHEN Shi-yue,LI Jun,YANG Yong.Trace element signatures of the Carboniferous -Permian deposits in the Bohai Gulf Basin and their facies significance[J].Sedimentary Geology and Tethyan Geology,2007,27(4):27-32. | |
| Authors: | MIAO Yao SANG Shu-xun LIN Hui-xi CHEN Shi-yue LI Jun YANG Yong |
| Institution: | 1. School of Resources and Geoscience, China University of Mining and Technology, Xuzhou 221008, J iangsu, China;2. Research Institute of Geological Sciences, Shengli Oil Field Corporation, Dongying 257015, Shandong, China;3. College of Geo-resources and Information, China University of Petroleum, Dongying 257000, Shandong, China |
| Abstract: | The present paper deals with the contents of the elements Sr, Ba, Ga, V, Ni and Co, and the ratios of Sr/Ba, Ba/Ga and Ni/Co analyzed by using ICP-MS technique for 42 pieces of the Carboniferous -Permian core samples from four wells in the Bohai Gulf Basin, and gives the following analyses:Sr=(100~200)×10-6, Ba=(100~700)×10-6, Ga=(10~40)×10-6, V=(80~200)×10-6, Co=(5~30)×10-6, Ni=(15~45)×10-6, Sr/Ba=0.2~0.9, Ba/Ga=2~20, Ni/Co=1~4. The results of research show that the marine deposits are developed in the Benxi Formation, the transitional deposits in the Taiyuan Formation, and the continental deposits in the Shanxi Formation and its overlying strata in the Bohai Gulf Basin. |
| Keywords: | Bohai Gulf Basin Carboniferous-Permian deposits trace element sedimentary facies |
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