末次冰期鄱阳湖西南缘地区的风尘堆积
鄱阳湖湖滨沙山是末次冰期特定气候条件下季风活动所产生的风成沙丘沉积体。在调查鄱阳湖沙山的过程中,发现位于鄱阳湖南部沙山下风方向的丰城-樟树-新余一带岗丘顶部几米厚的第四纪堆积地层,虽然颜色明显偏红,但地层性状及沉积学特征却与北方风成黄土及宁镇下蜀黄土有着很大的相似性。通过对具代表性的新余打鼓岭剖面进行分析,确认其成因系风力搬运而成的粉尘堆积。结合冬季风路径上沉积物粒度的空间变化特征,初步提出鄱阳湖沙山与新余一带风尘红土堆积是在末次冰期特定气候条件下,冬季风作用所形成的风沙-风尘堆积系统。鄱阳湖风成沙丘及其西南缘风尘沉积的发育是晚更新世末期江南鄱阳湖区气候环境恶化的佐证,也是对我国西北地区沙漠-...
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| Published in | Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 26; no. 1; pp. 101 - 108 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | Chinese |
| Published |
Beijing
Marine Geology and Quaternary Geology
01.01.2006
中国科学院地球环境研究所,黄土与第四纪地质国家重点实验室,西安,710075%南京大学,城市与资源学系,南京,210093%南京博物院,考古研究所,南京,210016 南京大学,城市与资源学系,南京,210093 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1492 |
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| Abstract | 鄱阳湖湖滨沙山是末次冰期特定气候条件下季风活动所产生的风成沙丘沉积体。在调查鄱阳湖沙山的过程中,发现位于鄱阳湖南部沙山下风方向的丰城-樟树-新余一带岗丘顶部几米厚的第四纪堆积地层,虽然颜色明显偏红,但地层性状及沉积学特征却与北方风成黄土及宁镇下蜀黄土有着很大的相似性。通过对具代表性的新余打鼓岭剖面进行分析,确认其成因系风力搬运而成的粉尘堆积。结合冬季风路径上沉积物粒度的空间变化特征,初步提出鄱阳湖沙山与新余一带风尘红土堆积是在末次冰期特定气候条件下,冬季风作用所形成的风沙-风尘堆积系统。鄱阳湖风成沙丘及其西南缘风尘沉积的发育是晚更新世末期江南鄱阳湖区气候环境恶化的佐证,也是对我国西北地区沙漠-黄土堆积过程的区域响应。 |
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| AbstractList | P534.63; 鄱阳湖湖滨沙山是末次冰期特定气候条件下季风活动所产生的风成沙丘沉积体.在调查鄱阳湖沙山的过程中,发现位于鄱阳湖南部沙山下风方向的丰城-樟树-新余一带岗丘顶部几米厚的第四纪堆积地层,虽然颜色明显偏红,但地层性状及沉积学特征却与北方风成黄土及宁镇下蜀黄土有着很大的相似性.通过对具代表性的新余打鼓岭剖面进行分析,确认其成因系风力搬运而成的粉尘堆积.结合冬季风路径上沉积物粒度的空间变化特征,初步提出鄱阳湖沙山与新余一带风尘红土堆积是在末次冰期特定气候条件下,冬季风作用所形成的风沙-风尘堆积系统.鄱阳湖风成沙丘及其西南缘风尘沉积的发育是晚更新世末期江南鄱阳湖区气候环境恶化的佐证,也是对我国西北地区沙漠-黄土堆积过程的区域响应. 鄱阳湖湖滨沙山是末次冰期特定气候条件下季风活动所产生的风成沙丘沉积体。在调查鄱阳湖沙山的过程中,发现位于鄱阳湖南部沙山下风方向的丰城-樟树-新余一带岗丘顶部几米厚的第四纪堆积地层,虽然颜色明显偏红,但地层性状及沉积学特征却与北方风成黄土及宁镇下蜀黄土有着很大的相似性。通过对具代表性的新余打鼓岭剖面进行分析,确认其成因系风力搬运而成的粉尘堆积。结合冬季风路径上沉积物粒度的空间变化特征,初步提出鄱阳湖沙山与新余一带风尘红土堆积是在末次冰期特定气候条件下,冬季风作用所形成的风沙-风尘堆积系统。鄱阳湖风成沙丘及其西南缘风尘沉积的发育是晚更新世末期江南鄱阳湖区气候环境恶化的佐证,也是对我国西北地区沙漠-黄土堆积过程的区域响应。 |
| Author | Zhi-yong, HAN Da-yuan, YANG Xu-sheng, LI Ying-san, FANG |
| AuthorAffiliation | 南京大学,城市与资源学系,南京,210093;中国科学院地球环境研究所,黄土与第四纪地质国家重点实验室,西安,710075%南京大学,城市与资源学系,南京,210093%南京博物院,考古研究所,南京,210016 |
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| Author_FL | LI Xu-sheng HAN Zhi-yong YANG Da-yuan FANG Ying-san |
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| Keywords | 风尘沉积 江西新余 末次冰期 鄱阳湖南部沙山 |
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| Snippet | 鄱阳湖湖滨沙山是末次冰期特定气候条件下季风活动所产生的风成沙丘沉积体。在调查鄱阳湖沙山的过程中,发现位于鄱阳湖南部沙山下风方向的丰城-樟树-新余一带岗丘顶部几米厚... P534.63; 鄱阳湖湖滨沙山是末次冰期特定气候条件下季风活动所产生的风成沙丘沉积体.在调查鄱阳湖沙山的过程中,发现位于鄱阳湖南部沙山下风方向的丰城-樟树-新余一带岗丘顶... |
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| SubjectTerms | Age Atmospheric particulates Beach erosion Climatic conditions Degeneration Desertification Dunes Dust Geosphere Grain size Hills Hydrosphere Lakes Loess Monsoons Pleistocene Quaternary Rivers Sand Sedimentary structures Wind Winter |
| Title | 末次冰期鄱阳湖西南缘地区的风尘堆积 |
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