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首页> 外文期刊>International Geology Review >Geochemical constraints on the origin and environment of Lower Cambrian, selenium-rich siliceous sedimentary rocks in the Ziyang area, Daba region, central China
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Geochemical constraints on the origin and environment of Lower Cambrian, selenium-rich siliceous sedimentary rocks in the Ziyang area, Daba region, central China

机译:中国中部大巴地区资阳地区下寒武统富硒硅质沉积岩成因与环境的地球化学约束

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摘要

The Ziyang area is one of the two major regions of central China subjected to selenium (Se) poisoning. Systematic studies of Se contents of different lithologies from this area indicate that Lower Cambrian, carbonaceous, and siliceous strata host the highest Se contents (with Se contents of up to 278 ppm). We have investigated their geochemical characteristics (major and trace elements, and Si and O isotopes), origin, and sedimentary environment of formation. The siliceous rocks are characterized by a wide range in major elements, and are enriched in Se, Ba, Cu, Ni, V, As, Sb, and U relative to average continental crust. They are also enriched in light rare earth elements relative to heavy rare earth elements (LaN/YbN = 1.64-35.7) and show weak or moderate negative Ce anomalies and strong positive Eu anomalies. δ30SiNBS-28 and δ18OV-SMOW values range from -0.3‰ to 0.6‰ and 16.1‰ to 21.7‰, respectively. The homogenization temperatures of inclusions within the studied samples range from 113°C to 319°C, and their salinities from 1.2 to 13.7 wt.% NaCl equivalent. Our results suggest that the studied siliceous rocks resulted from hydrothermal sedimentation in a relatively anoxic semi-deep sea sedimentary environment. The hydrothermal fluid responsible for Se-mineralization involved the mixing of low-temperature high-salinity fluid, low-temperature low-salinity fluid, and a high-temperature low-salinity basinal fluid in the NaCl-(KCl)-H2O system.View full textDownload full textKeywordssiliceous rocks, selenium content, sedimentary environment, Shaanxi Province, ChinaRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00206814.2011.580625
机译:资阳地区是中国中部遭受硒中毒的两个主要地区之一。该地区不同岩性的硒含量的系统研究表明,下寒武统,碳质和硅质地层的硒含量最高(硒含量最高为278 ppm)。我们研究了它们的地球化学特征(主要和微量元素,以及Si和O同位素),成因和沉积环境。硅质岩的主要元素特征广泛,相对于平均陆壳而言,其富含硒,钡,铜,镍,钒,砷,锑和铀。他们还相对于重稀土元素(La N / Yb N == 1.64-35.7)富含轻稀土元素,并且显示出弱或中度Ce负异常和强正Eu异常。 α 30 Si NBS-28 和α 18 O V-SMOW 的值范围为-0.3 °分别为0.6到16.1到21.7。研究样品中夹杂物的均质温度范围为113°C至319°C,盐度为1.2至13.7 wt。%NaCl当量。我们的结果表明,研究的硅质岩是在相对缺氧的半深海沉积环境中由热液沉积形成的。负责矿化作用的热液涉及在NaCl-(KCl)-H 中混合低温高盐度流体,低温低盐度流体和高温低盐度盆地流体2 系统。 ,linkedin,facebook,stumbleupon,digg,google,更多”,发布号:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2011.580625

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