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2.
余学义 《西安科技大学学报》1996,(4)
通过分析地下开采的影响,黄土覆盖层变形裂缝规律,提出以开采方法和工艺方式来控制或减弱地表变形裂缝破坏程度,并在保护地表建筑物的前提下,最大限度回收“三下”呆滞煤炭 相似文献
3.
4.
文章介绍了黄土湿陷性试验的两种试验方法,对黄土湿陷机理作了简要分析,并对双线法的误差及其修正进行了讨论。 相似文献
5.
A recording phase lag between ocean and continent climate changes: Constrained by the Matuyama/Brunhes polarity boundary 总被引:6,自引:0,他引:6
The Matuyama/Brunhes polarity boundary (MBPB) is recorded in Chinese loess L8, which is associated with the glacial period.
It is proved that loess L8 is capable of recording earth’s secular variation, and the lock-in depth in Chinese loess is no
more than that of marine sediments. Comparison with the location of MBPB in Chinese loess and marine sediments, it is put
forward that there is a recording phase lag between ocean and continent climate changes. 相似文献
6.
In the transitional region between the Loess Plateau and deserts, 4 sections located respectively at Yuling, Hengshan, Dingbian
and Huining of China are studied. The high-resolution paleoclimatic records obtained show that environmental events on varying
time scales have happened over East Asia. These events are dated with the time scales established using the recently-developed
approach of Automatic Orbital Tuning. This leads to the establishment of the chronology of the environmental events. 相似文献
7.
王银梅 《太原理工大学学报》1998,29(1):95-98
在分析资料和室内试验的基础上,概括了提高水泥黄土强度有效措施,就水泥黄土硬化和外加剂对水泥黄土的作用机理进行了初步探讨。 相似文献
8.
中国黄土区东亚古季风气候与冰期气候对比研究 总被引:2,自引:0,他引:2
岳乐平 《西北大学学报(自然科学版)》1998,28(2):157-162
研究了中国黄土区冰期气候与季风气候记录;进行了黄土磁化率与大洋δ18O曲线对比,并且将黄土组合—古土壤组合与冰期-间冰期气候进行了比较。结果表明:黄土组合与古土壤组合记录了冰期气候与间冰期气候;中国黄土—古土壤堆积是全球冰期—间冰期气候变化与东亚古季风气候变化共同作用的结果。 相似文献
9.
THE COMPARISON OF LANZHOU LOESS PROFILE WITH VOSTOK ICE CORE IN ANTARCTICA OVER THE LAST GLACIATION CYCLE 总被引:4,自引:0,他引:4
Loess near Lanzhou in the late Pleistocene is very sensitive to climatic fluctuations. The Beiyuan terrace profile in Linxia City, of which the curve of susceptibility tallies with the trend of isotopic curves of Vostok 2083 m ice core in Antarctica, is 35m thick. There are five layers of paleosols under Malan loess(L_1). Upper three layers (S_(1-a),S(1-b)and S_(1-c) correspond to three warm stages in last interglaciation, Interstadial of Last Glacial (C stage in Antarctic ice core)was clearly recorded in the Beiyuan profile, in which three layers of paleosols and two of loess were formed. The lowest section of the profile belongs to penultimate glaciation, in which fossils of cold-drought-resistant mammal and mollusc have been discovered. 相似文献
10.
Loess-soil sequences in southern Anhui Province: Magnetostratigraphy and paleoclimatic significance 总被引:8,自引:0,他引:8
QIAOYansong GUOZhengtang HAOQingzhen WUWenxiang JIANGWenying YUANBaoyin ZHANGZhongshi WEIJianjing ZHAOHua 《科学通报(英文版)》2003,48(19):2088-2093
Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP. 相似文献