北黄海浅表层沉积物微量元素的分布及其早期成岩作用探讨
P736.4; 探讨北黄海早期成岩过程中微量元素的分布特征及其对古环境判别指标的影响,结果显示,沉积物中微量元素分布主要受陆源碎屑控制, 而早期成岩过程对这种受源岩控制的微量元素分布特征影响不大.早期成岩作用对Mn、Ni、V、Zn影响剧烈.U/Th、V/Cr比值表明古底层水环境为氧化环境,V/(V+Ni)比值揭示底层水为厌氧环境,这与V、Ni受早期成岩作用影响较大有关,其不能真实地记录古底层水的氧化还原环境....
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| Published in | Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 27; no. 3; pp. 43 - 50 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | Chinese |
| Published |
Beijing
Marine Geology and Quaternary Geology
01.01.2007
中国科学院,研究生院,北京,100039%中国科学院,研究生院,北京,100039%青岛海洋地质研究,青岛,266071 海洋沉积与环境地质国家海洋局重点实验室,国家海洋局,第一海洋研究所,青岛,266061 中国科学院,海洋研究所,青岛,266071 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1492 |
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| Abstract | P736.4; 探讨北黄海早期成岩过程中微量元素的分布特征及其对古环境判别指标的影响,结果显示,沉积物中微量元素分布主要受陆源碎屑控制, 而早期成岩过程对这种受源岩控制的微量元素分布特征影响不大.早期成岩作用对Mn、Ni、V、Zn影响剧烈.U/Th、V/Cr比值表明古底层水环境为氧化环境,V/(V+Ni)比值揭示底层水为厌氧环境,这与V、Ni受早期成岩作用影响较大有关,其不能真实地记录古底层水的氧化还原环境. |
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| AbstractList | 探讨北黄海早期成岩过程中微量元素的分布特征及其对古环境判别指标的影响,结果显示,沉积物中微量元素分布主要受陆源碎屑控制,而早期成岩过程对这种受源岩控制的微量元素分布特征影响不大。早期成岩作用对Mn、Ni、V、Zn影响剧烈。U/Th、V/Cr比值表明古底层水环境为氧化环境,V/(V+Ni)比值揭示底层水为厌氧环境,这与V、Ni受早期成岩作用影响较大有关,其不能真实地记录古底层水的氧化还原环境。 P736.4; 探讨北黄海早期成岩过程中微量元素的分布特征及其对古环境判别指标的影响,结果显示,沉积物中微量元素分布主要受陆源碎屑控制, 而早期成岩过程对这种受源岩控制的微量元素分布特征影响不大.早期成岩作用对Mn、Ni、V、Zn影响剧烈.U/Th、V/Cr比值表明古底层水环境为氧化环境,V/(V+Ni)比值揭示底层水为厌氧环境,这与V、Ni受早期成岩作用影响较大有关,其不能真实地记录古底层水的氧化还原环境. |
| Author | Xue-fa, SHI Shuang-lin, LI ZOU Jian-jun |
| AuthorAffiliation | 中国科学院,海洋研究所,青岛,266071;海洋沉积与环境地质国家海洋局重点实验室,国家海洋局,第一海洋研究所,青岛,266061;中国科学院,研究生院,北京,100039%中国科学院,研究生院,北京,100039%青岛海洋地质研究,青岛,266071 |
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| Author_FL | LI Shuang-lin ZOU Jian-jun SHI Xue-fa |
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| SubjectTerms | Anoxia Anoxic conditions Anoxic sediments Diagenesis Manganese Oxic conditions Ratios Sediment Sediments Zinc |
| Title | 北黄海浅表层沉积物微量元素的分布及其早期成岩作用探讨 |
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