| 中国湖相碳酸盐岩碳氧同位素时空特征及其古湖泊学意义 |
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| 引用本文： | 梁俊红,孙宝亮,尹国英.中国湖相碳酸盐岩碳氧同位素时空特征及其古湖泊学意义[J].地质找矿论丛,2022,37(4):469-483. |
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| 作者姓名： | 梁俊红 孙宝亮 尹国英 |
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| 作者单位： | 东北大学资源与土木工程学院地质系, 沈阳 110819;辽宁城市建设职业技术学院建筑工程系, 沈阳 110122 |
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| 基金项目： | 中央高校基本科研业务费项目(编号:N100401005)资助。 |
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| 摘 要： | 湖相碳酸盐岩是一种分布极其广泛的陆相碳酸盐岩。中国湖相碳酸盐岩沉积始于二叠纪—三叠纪,经侏罗纪—白垩纪发展,鼎盛于古近纪,具有沉积时间跨度长、分布面积广的特征。碳酸盐岩发育方式多样,常以多个单层、薄夹层状、互层状、韵律沉积为主,也见以结核状或钙质微体化石等薄层赋存于泥岩、页岩等细粒碎屑岩中。湖相碳酸盐岩δ13C值介于-10.0×10-3~+10.0×10-3之间,多数为-5.0×10-3~+5.0×10-3,正负值均有。二叠系—三叠系δ13C发生负偏,侏罗系—白垩系先正向漂移随后负偏,古近系—新近系再次正偏,达最大值约+5.0×10-3。氧同位素δ18O值介于-20.0×10-3~+2.0×10-3之间,多数为-15.0×10-3~-0.0×10-3,几乎全部为负值。二叠系—三叠系、侏罗系—白垩系碳酸盐岩δ18O值在-15.0×10-3~-3.0×10-3之间变化,古近系—新近系δ18O值明显正偏移,多数位于-10.0×10-3~0.0×10-3。中国湖相碳酸盐岩碳氧同位素相关性分析表明,δ13C与δ18O密切相关,且δ13C值多正值或轻微负值,指示湖泊为封闭型咸水—半咸水环境;δ13C和δ18O不相关,δ13C值为负值,指示湖泊为开放型淡水环境。
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| 关 键 词： | 湖相碳酸盐岩 岩石学 碳氧同位素 古湖泊学 |
| 收稿时间： | 2022/5/6 0:00:00 |
Temporal and spatial characteristics of C-O isotopes of Lacustrine carbonate in China and the Paleolimnological significance |
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| LIANG Junhong,SUN Baoliang,YIN Guoying.Temporal and spatial characteristics of C-O isotopes of Lacustrine carbonate in China and the Paleolimnological significance[J].Contributions to Geology and Mineral Resources Research,2022,37(4):469-483. |
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| Authors: | LIANG Junhong SUN Baoliang YIN Guoying |
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| Institution: | Geology Department of school of Resources and civil Engineering of The Northeast University, Shenyang 110819, China; Structural Engineering department of Liaoning Urban Construction Technical College, Shenyang 110122, China |
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| Abstract: | Lacustrine carbonate rock is a widely distributed continental facies. In China it is also widely distributed and precipitated in long terms beginning in Permian-Triassic period, developing in Jurassict-Cretaceous period and flourishing in Paleogene. It occurs in different forms, such as the dominant rhythmic multi-single layers, thin intercalith and interbeded layers, thin nodular and calcareous micro-fossil layers in mudstone or shale. The value is in range -10.0×10-3~+10.0×10-3 and most of the value in range -5.0×10-3~+5.0×10-3 in Permian-Triassic period tends to be negative, in Jurassic-Cretaceous period first to be positive and then negative, in Paleogene to be positive with top value +5.0×10-3. The value is in range -20.0×10-3~+2.0×10-3 and most of the value in range -15.0×10-3~0.0×10-3 of which almost are negative. The value of Permian-Triassic period and Jurassic-Cretaceous period is in range -15.0×10-3~-3.0×10-3, the value of Paleogene -10.0×10-3~0.0×10-3 tend to be positive. Analysis of correlation of C and O isotopes shows that and are closely correlated and most positive, slightly negative indicating that the lakes is under closed environment with saline-semisaline water, are not correlated and value negative indicating that the lakes under open environment with fresh water. |
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| Keywords: | lacustrine carbonate petrology C-O isotopes paleolimnology |
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