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OALib Journal期刊
ISSN: 2333-9721
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东亚沿海山地末次冰期冰川与环境
DOI: 10.11821/xb200901004, PP. 33-42
Keywords: 东亚山地,末次冰期,冰川环境,构造背景
Abstract:
对东亚沿海山地末次冰期冰川发育的气候条件、构造背景、冰进时序、发育规模等研究表明，台湾山地保存着3期冰川作用遗迹，冰川的最大前进规模发生在MIS3b阶段，其规模大于MIS2阶段；日本山地冰期系列齐全，包含了末次冰期的早(MIS4)、中(MIS3)、晚(MIS2)3个阶段的冰进，其规模是MIS4/3阶段大于MIS2阶段；而长白山存在2期冰川作用的遗迹，即末次冰盛期(MIS2)和晚冰期。在相似的冬雨(雪)型季风影响区，冰川发育的时序与规模也有一定不同，反映出在大气候背景下的区域性差异，在东亚季风影响范围内，末次冰期的环流变化在各地也很不一致。最新推算的现代理论雪线自北(日本)向南(台湾)依次递增，范围是2750~4245m，除日本北部的高纬地区雪线降低值400m之外，末次冰盛期(LGM)的雪线降低值在800~1300m之间，平均值1000m左右。东亚沿海山地冰川发育与新构造运动密切相关，更新世山体的快速抬升为冰川发育的内因，如台湾山地在末次冰期的MIS3b阶段，山体的抬升量约为250m，对山体的高度和雪线变化有很大影响。
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