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黄河源区第四纪地层及古地理环境演化探讨 被引量:22
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作者 王绍令 李位乾 《冰川冻土》 CSCD 北大核心 1992年第1期45-54,共10页
根据第四纪地层及各类试验资料,重建本区第四纪以来古地理环境及演化过程。早更新世时为温、湿的森林草原环境;中更新世时气候从温、湿向冷、干演化,形成查哈西里冰期;晚更新世时气候继续变冷,出现冰期和间冰期交替,早期为哈拉滩冰期,... 根据第四纪地层及各类试验资料,重建本区第四纪以来古地理环境及演化过程。早更新世时为温、湿的森林草原环境;中更新世时气候从温、湿向冷、干演化,形成查哈西里冰期;晚更新世时气候继续变冷,出现冰期和间冰期交替,早期为哈拉滩冰期,中期为间冰期,晚期为布尔汉布达山冰期,期间经历了疏林草原—草原环境交替演化过程;全新世时处于冷、干的冰缘气候下的草原环境。 展开更多
关键词 地层 古地理环境 第四纪 黄河源区
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黄河源头区首次发现深埋藏湖冰 被引量:6
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作者 王绍令 李位乾 《冰川冻土》 CSCD 北大核心 1990年第3期201-207,共7页
黄河源头鄂陵湖北岸CK6孔深19.81—24.26m段发现厚4.45m的纯冰层,对冰样及其上下地层的土样、水样化验及对湖周围地貌、第四纪的研究结果表明,厚层冰属深埋藏湖冰,生成年代为距今35030—45209年,成冰时的年平均气温约-10℃。
关键词 深埋藏 湖冰 古气候 黄河源头区
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THE DISCOVERED DEEP BURIED LAKE ICE IN SOURCE REGION OF THE HUANGHE RIVER
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作者 王绍令 李位乾 《Chinese Geographical Science》 SCIE CSCD 1993年第3期57-64,共8页
The 4.45 m-thick pure ice lens have been discovered firstly at depth from 19.81 -24.26 m in the bore No.6, which locates in north bank of the Ngoring Lake. In source region of the Huanghe (Yellow) River, 14C dating, X... The 4.45 m-thick pure ice lens have been discovered firstly at depth from 19.81 -24.26 m in the bore No.6, which locates in north bank of the Ngoring Lake. In source region of the Huanghe (Yellow) River, 14C dating, X -ray diffraction, pollen analysis, micropalaeontology, chemical components, environmental isotope 2H, 3H, 18O and freezing point of the ice and water samples from the bore have been tested and microorganism in the ice have been also appraised with microscope. Combined with the research on geomorphy and Quaternary around the lake, the ice lens are determined as a kind of deep-buried lake ice, formed in 35,030-45,209 yr.B.P., and annual mean air temperature was about -10℃ during that time. 展开更多
关键词 source region of the Huanghe RIVER deep-buried LAKE ICE PALAEOCLIMATE
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