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台湾野柳微地貌成因分析

赵松龄

海洋科学2016,Vol.40Issue(6):72-76,5.
海洋科学2016,Vol.40Issue(6):72-76,5.DOI:10.11759/hykx20150928002

台湾野柳微地貌成因分析

Analysis of the cause of Yehliu microgeomorphology, Taiwan

赵松龄1

作者信息

  • 1. 中国科学院海洋研究所,山东 青岛 266071
  • 折叠

摘要

Abstract

To understand paleoglaciation in Eastern China from a spatial perspective, the author participated in the 16th Cross-Strait Symposium on topography in September, 2015. Through a field investigation in the Yeliu area, Taiwan Island, the author confirmed that microgeomorphology with grouped Moulin in the Yeliu area belongs to the low-latitude-type glaciation. The finding indicates that glaciation occurred in the last glacial period both in Eastern China and northern Taiwan Island, leaving broadly distributed glacial relics.

关键词

湾流/黑潮/野柳/古冰川/中国台湾

Key words

gulf stream/the Kuroshio/Yeliu area/ancient glaciers/Taiwan

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资源环境

引用本文复制引用

赵松龄..台湾野柳微地貌成因分析[J].海洋科学,2016,40(6):72-76,5.

海洋科学

OA北大核心CSCDCSTPCD

1000-3096

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