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大营地区古层间氧化带识别与空间定位预测

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鲁超, 焦养泉, 彭云彪, 吴立群, 苗爱生, 荣辉, 谢惠丽. 2018. 大营地区古层间氧化带识别与空间定位预测[J]. 中国地质, 45(6): 1228-1240. doi: 10.12029/gc20180612
引用本文: 鲁超, 焦养泉, 彭云彪, 吴立群, 苗爱生, 荣辉, 谢惠丽. 2018. 大营地区古层间氧化带识别与空间定位预测[J]. 中国地质, 45(6): 1228-1240. doi: 10.12029/gc20180612
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LU Chao, JIAO Yangquan, PENG Yunbiao, WU Liqun, MIAO Aisheng, RONG Hui, XIE Huili. 2018. Paleo-interlayer oxidation zone identification and spatial localization prediction in Daying area[J]. Geology in China, 45(6): 1228-1240. doi: 10.12029/gc20180612
Citation: LU Chao, JIAO Yangquan, PENG Yunbiao, WU Liqun, MIAO Aisheng, RONG Hui, XIE Huili. 2018. Paleo-interlayer oxidation zone identification and spatial localization prediction in Daying area[J]. Geology in China, 45(6): 1228-1240. doi: 10.12029/gc20180612
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大营地区古层间氧化带识别与空间定位预测

  • 1.

    中国地质大学, 湖北 武汉 430074

  • 2.

    核工业二〇八大队, 内蒙古 包头 014010

  • 基金项目: 国家重点基础研究发展计划"973"项目"中国北方巨型砂岩铀成矿带陆相盆地沉积环境与大规模成矿作用"（2015CB453000）、鄂尔多斯盆地北缘含铀岩系三维地质编图项目（12120115013701）和鄂尔多斯盆地北部古层间氧化带特征分析及远景预测评价项目（核工业地质局）资助成果
详细信息
    作者简介: 鲁超, 男, 1984年生, 博士生, 从事砂岩型铀矿科研和生产工作; E-mail:56709507@qq.com

  • 中图分类号: P619.14;P588.2

Paleo-interlayer oxidation zone identification and spatial localization prediction in Daying area

  • 1.

    China University of Geosciences, Wuhan 430074, Hubei, China

  • 2.

    No. 208 Geological Party, CNNC, Baotou 014010, Inner Mongolia, China

  • Fund Project: supported by National basic research program of China "973" Project, Sedimentary environment and large scale mineralization of continental basins in giant sandstone uranium metallogenic belt in North China (No. 2015CB453000), and threedimensional geological mapping of uranium bearing rocks on the northern margin of Ordos Basin project (No. 12120115013701)
More Information
    Author Bio: LU Chao, male, born in 1984, master candidate, engages in the study of uranium geology; E- mail: 56709507@qq.com .

    摘要

  • 潜在铀储层内部的层间氧化作用与铀成矿作用同时进行而且密不可分，（古）层间氧化带被认为是砂岩型铀矿的重要找矿标志。运用岩芯和钻孔资料以及各分带的岩石矿物学以及地球化学特征等信息识别古层间氧化带，结合铀储层中具有古氧化性质和还原性质的岩石地球化学标志，定量地给予古层间氧化带以空间定位，并据此可以划分出古完全氧化带、过渡带和还原带。在此基础上，探讨了铀储层规模、隔挡层、暗色泥岩及煤层等因素对于古层间氧化带分布的影响。

    Interlayer oxidation in potential uranium reservoir is closely related to uranium mineralization. Paleo-interlayer oxidation zone is considered to be an important symbol in search for sandstone type uranium deposits. In this paper, core drilling data and mineralogy and geochemical characteristics of each sub-band of interlayer oxidation were used to identify the paleo-interlayer oxidation. Combined with paleo-oxidic and reductive properties of uranium geochemical markers in uranium reservoirs, paleointerlayer oxidation was spatial positioned quantitatively. Accordingly, paleo-completely-oxidized zone and transitional zone and reduction zone were divided and identified. On such a basis, the distribution of paleo-interlayer oxidation zone controlled by the scale of the uranium reservoir, barrier layers, the dark mudstone and coal seam and other factors was discussed.

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  • 图 1  鄂尔多斯盆地北东部铀矿地质图（附大营地区位置）

    Figure 1. 

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    图 2  大营地区典型古氧化-还原带砂岩宏观岩石学特征照片

    Figure 2. 

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    图 3  大营地区典型古氧化-还原带微观岩石学特征照片

    Figure 3. 

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    图 4  大营地区直罗组下段下亚段和下段上亚段氧化带空间分布图

    Figure 4. 

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    图 5  大营地区直罗组下段下亚段和下段上亚段古层间氧化带的控制因素

    Figure 5. 

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    图 6  大营西地区直罗组下段古层间氧化带与铀矿化分布规律走向剖面图

    Figure 6. 

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    表 1  大营地区陆源碎屑及填隙物组分在不同氧化分带中的特征

    Table 1.  Terrigenous clastic and interstitial materials component characteristics in different oxidation zones in Daying area

    下载: 导出CSV

    表 2  大营地区不同类型砂岩的环境敏感参数对比

    Table 2.  Comparison of environmentally sensitive parameters of different types of sandstone in Daying area

    下载: 导出CSV
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收稿日期:  2016-10-31
修回日期:  2017-01-25
刊出日期:  2018-12-25

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