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OALib Journal期刊
ISSN: 2333-9721
费用：99美元
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汾河流域地貌发育对构造运动和气候变化的响应
DOI: 10.11821/xb200203007, PP. 310-318
Keywords: 冲湖积台地,碳酸钙结晶体,黄土古土壤序列,第四纪,地貌响应,汾河流域
Abstract:
自中更新世中晚期以来,由于构造运动及气候变化,在汾河流域系列盆地中无论是地貌还是沉积都出现了相应的变化。根据对系列盆地中普遍发育的三级冲湖积台地的成因分析,发现发生于0.76MaBP、0.55MaBP及0.13MaBP的3次大幅度区域构造抬升是导致古湖盆湖退、三级台地形成的根源。根据对太原盆地东南边缘的一台地-洪山台地湖积层的分析,发现在相邻两次构造抬升之间的构造相对稳定期,气候变化完全控制着湖盆的演化。由第四纪气候的干湿变化对象太原盆地这样大的湖盆,一般只引起不大于4.5m的湖面升降,与构造抬升引起的湖面变动相差甚大。作为影响河湖地貌发育的2个主导因素,构造运动是主要的,气候变化只是在构造稳定期才突出地显示其影响。
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