Paleolake alteration research of southeast Shandong since Holocene based on GIS

The Shandong southwest area is located on the fracture zone connecting Shandong hills and north china plain. Since Holocene, affected by development of Huanghe alluvial fan, Zhanghe alluvial fan and Hutuhe alluvial fan, a coastal lagoon was formed in the low-lying area of Huanghe alluvial fan. Under...

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Bibliographic Details
Published in2011 19th International Conference on Geoinformatics pp. 1 - 4
Main Authors Handong He, Anbo Li
Format Conference Proceeding
LanguageEnglish
Published IEEE 01.06.2011
Subjects
climate change
Geology
Huanghe alluvial fan
Humans
Lakes
Meteorology
Ocean temperature
paleoenvironment
paleolakes
Remote sensing
Rivers
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Summary:The Shandong southwest area is located on the fracture zone connecting Shandong hills and north china plain. Since Holocene, affected by development of Huanghe alluvial fan, Zhanghe alluvial fan and Hutuhe alluvial fan, a coastal lagoon was formed in the low-lying area of Huanghe alluvial fan. Under the influence of the development of Huanghe alluvial fan, climate change in north china and human activity, paleolakes in Shandong southeast area appeared in different levels of development and shapes in times of early Holocene, Holocene and late Holocene. Referring to the record information of lake terraces on 1 Ka.B.P and measuring spots of JiediI, Huyan, Zhakou, Doumen, and Shuiba which could reflect geographic boundaries of the lakes, we are able to recover the geographic paleoenvironment of the lakes 1Ka.B.P.
ISBN:1612848494
9781612848495
ISSN:2161-024X
DOI:10.1109/GeoInformatics.2011.5981093