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Formation mechanisms and significance of saline-lacustrine Se-rich soils in the Xining Basin |
ZHANG Ya-Feng1( ), JI Bing-Yan2( ), SHEN Xiao1, YAO Zhen1, MA Qiang1, WANG Shuai1, HE Lian-Zhen1, HAN Wei-Ming1 |
1. The Fifth Geological Exploration Institute of Qinghai Province, Xining 810099,China 2. The Fourth Geological Exploration Institute of Qinghai Province, Xining 810000,China |
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Abstract As shown by the investigation and analysis of the Se content in soils and rocks of the Xining Basin, the rocks and soils in the Paleogene Xining Formation and the Cretaceous Minhe Formation have the highest Se content, which makes them the major Se-rich parent materials of soils in the basin. By combining the paleogeographic data on the retreating process of the basin, it can be concluded that the Paleogene Xining Formation and the Neogene Guide Group were deposited from the arid and hot saline lacustrine facies to the humid and cool saline-freshwater lacustrine facies. The combined action of the saline lake boundary and the arid and hot saline-lacustrine environment, as well as the following transformation by landforms and water systems, contributed to the formation of the existing framework of saline-lacustrine sedimentary Se-rich soils in the Xining Basin. Such Se-rich soils enjoy the advantages of a low heavy metal content, a moderate Se content, and a high available Se content and thus are of great value in development and utilization.
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Received: 24 June 2022
Published: 27 April 2023
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Geological map of the Xining Basin
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地质单元 | 样品数 | 平均值/10-6 | 离差/10-6 | 变异系数 | 第四系 | 2587 | 0.28 | 0.14 | 0.51 | 古近系 | 2074 | 0.33 | 0.39 | 1.19 | 新近系 | 13 | 0.22 | 0.14 | 0.63 | 白垩系 | 472 | 0.29 | 0.25 | 0.86 | 古生界 | 67 | 0.15 | 0.05 | 0.33 | 元古宇 | 189 | 0.26 | 0.13 | 0.48 | 侵入岩 | 49 | 0.20 | 0.09 | 0.47 | 全区 | 5486 | 0.28 | 0.27 | 0.97 |
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Statistics of selenium content of soil in different geological units in the Xining Basin
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Distribution of soil selenium in the Xining Basin
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序号 | 取样地区 | 地层 | 岩性 | Se含量值/10-6 | 1 | 乐都区高店南 | 新近系贵德群 | 红色泥岩 | 0.14 | 2 | 互助县北硝沟 | 古近系西宁组 | 红色泥岩 | 0.87 | 3 | 平安区洪水泉 | 古近系西宁组 | 红色泥岩 | 0.64 | 4 | 平安区石沟沿 | 古近系西宁组 | 红色泥岩 | 0.95 | 5 | 平安区小峡镇 | 白垩系民和组 | 棕红色砂岩 | 0.73 | 6 | 平安区石灰窑 | 白垩系民和组 | 棕红色泥岩 | 0.20 | 7 | 乐都区汉庄北 | 古元古界东岔沟组 | 石英砂岩 | 0.13 | 8 | 乐都区吴家台 | 长城系青石坡组 | 青灰色砂岩 | 0.15 | 9 | 乐都区晁家南 | 奥陶系二长花岗岩 | 二长花岗岩 | 0.05 | 10 | 平安区白草湾 | 志留系花岗闪长岩 | 花岗闪长岩 | 0.04 |
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Selenium content of rocks in different strata in the Xining Basin
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