High-resolution analysis of early diagenetic effects on magnetic;minerals in post-middle-Holocene continental shelf sediments from the;Korea Strait | |
Liu, J5; Zhu, RX; Roberts, AP; Li, SQ; Chang, JH | |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH |
2004 | |
卷号 | 109期号:B3;AR B03103页码:- |
关键词 | magnetite diagenesis continental shelf sediments rock magnetism post-middle Holocene Korea Strait |
ISSN号 | 0148-0227 |
DOI | 10.1029/2003JB002813 |
英文摘要 | Two studied sediment cores from the Korea Strait contain mud sequences ( 14 m and 32.62 m in thickness) that were deposited during the last 6,000 years. The sediments have uniform lithology and geochemical properties, however, marked down-core changes in magnetic properties suggest that diagenesis has significantly impacted the magnetic properties. An expanded view of early diagenetic reactions that affect magnetic mineral assemblages is evident in these rapidly deposited continental shelf sediments compared to deep-sea sediments. The studied sediments are divided into four descending intervals, based on magnetic property variations. Interval 1 is least affected by diagenesis and has the highest concentrations of detrital magnetite and hematite, and the lowest solid-phase sulfur contents. Interval 2 is characterized by the presence of paramagnetic pyrite and sharply decreasing magnetite and hematite concentrations, which suggest active reductive dissolution of detrital magnetic minerals. Interval 3 is marked by a progressive loss of hematite with depth, and coincides with the minimum magnetite concentration. Interval 4 has an increasing down-core enhancement of authigenic greigite, which apparently formed at depths of 3-30 m below the sediment-water interface due to arrested pyritization reactions. These results indicate delays of thousands of years for acquisition of magnetizations carried by greigite, which suggests that studies of geomagnetic field behavior from greigite-bearing continental shelf sediments should be conducted with care. Also, virtually complete destruction of detrital magnetic minerals at depth suggests that magnetic studies of rapidly deposited shelf sediments are unlikely to provide a meaningful signature associated with syndepositional environmental processes. |
学科主题 | 第四纪地质 |
WOS关键词 | ANOXIC MARINE-SEDIMENTS ; SEA-LEVEL CHANGES ; HEMIPELAGIC SEDIMENTS ; YELLOW SEA ; ENVIRONMENTAL MAGNETISM ; HYSTERESIS PROPERTIES ; SOUTHWESTERN ; TAIWAN ; BEARING SEDIMENTS ; ROCK MAGNETISM ; GREIGITE FE3S4 |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | AMER GEOPHYSICAL UNION |
WOS记录号 | WOS:000220433900003 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/37655] |
专题 | 中国地质调查局青岛海洋地质研究所 |
作者单位 | 1.China Geol Survey, Qingdao Inst Marine Geol, Qingdao 266071, Peoples R China. 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China. 3.Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England. 4.Korean Inst Geol Min & Mat, Taejon 305350, South Korea. 5.中国地质调查局青岛海洋地质研究所 |
推荐引用方式 GB/T 7714 | Liu, J,Zhu, RX,Roberts, AP,et al. High-resolution analysis of early diagenetic effects on magnetic;minerals in post-middle-Holocene continental shelf sediments from the;Korea Strait[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2004,109(B3;AR B03103):-. |
APA | Liu, J,Zhu, RX,Roberts, AP,Li, SQ,&Chang, JH.(2004).High-resolution analysis of early diagenetic effects on magnetic;minerals in post-middle-Holocene continental shelf sediments from the;Korea Strait.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,109(B3;AR B03103),-. |
MLA | Liu, J,et al."High-resolution analysis of early diagenetic effects on magnetic;minerals in post-middle-Holocene continental shelf sediments from the;Korea Strait".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 109.B3;AR B03103(2004):-. |
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