共查询到20条相似文献,搜索用时 232 毫秒
1.
Baochong Chen 《中国地理科学(英文版)》1994,4(3):242-251
陈宝冲THECHANGEOFTHEGENERALFORMANDTHETRANSPORTOFTHEWATER,LOADANDSALTABOUTTHENORTH-BRANCHOFTHECHANGJIANGRIVERMOUTH¥ChenBaochong(N... 相似文献
2.
EVOLUTIONOFRAPIDSOFCREEKMOUTH-BARATGEZHOUBARESERVOIRANDTHEIMPACTSONNAVIGABLECHANNELINTHEUPPERREACHESOFTHECHANGJIANGRIVER¥LinC... 相似文献
3.
THE VERTICAL DISTRIBUTION OF AGROTOPOCLIMATIC RESOURCES IN THE WARM SECTORS OF THE THREE GORGES AREA OF THE CHANGJIANG RIVER 总被引:1,自引:0,他引:1
罗洪,邓先瑞THEVERTICALDISTRIBUTIONOFAGROTOPOCLIMATICRESOURCESINTHEWARMSECTORSOFTHETHREEGORGESAREAOFTHECHANGJIANGRIVER¥DengXianrui;... 相似文献
4.
THE ORIGIN AND CHARACTERISTICS OF THE GLACIAL DEBRIS FLOW IN THE DUKU HIGHWAY OF TIANSHAN MOUNTAINS,
THEORIGINANDCHARACTERISTICSOFTHEGLACIALDEBRISFLOWINTHEDUKUHIGHWAYOFTIANSHANMOUNTAINS,CHINA¥XiongHeigang(DepartmentofGeography... 相似文献
5.
Qihao Weng 《中国地理科学(英文版)》1994,4(4):303-309
(翁齐浩)THERELATIONSHIPBETWEENTHEENVIRONMENTALCHANGEOFTHEZHUJIANGRIVERDELTAINHOLOCENEANDITSCULTURALORIGINSANDPROPAGATION¥WengQih... 相似文献
6.
Wang Lilun 《中国地理科学(英文版)》1996,6(4):304-312
THE CONDITIONS OF THE GLACIAL WATER RESOURCE AND WAYS OF ITS EXPLOITATION AND UTILIZATION IN CHINATHECONDITIONSOFTHEGLACIALWA... 相似文献
7.
INFLUENCEOFSEA-AIRINTERACTIONONTHEDISCHARGEOFFLOODSEASONINTHEUPPERREACHESOFTHECHANGJIANGRIVERZhangXinping(章新平)(LanzhouInstitu... 相似文献
8.
ANANALYSISOFWATERRESOURCECHARACTERISTICSOFTHERIVERSINTHENORTHERNSLOPEOFTHEKUNLUNMOUNTAINSXuYoupeng(许有鹏);GaoYunjue(高蕴珏)(Depart... 相似文献
9.
THEHOLOCENESEDIMENTALCHARACTERISTICANDPALEOCLIMATICEVOLUTIONOFEBINURLAKE,XINJIANG吴敬禄,王苏民,吴艳宏THEHOLOCENESEDIMENTALCHARACTERIST... 相似文献
10.
Li Xiaojian 《中国地理科学(英文版)》1996,(4)
HONG KONG DIRECT INVESTMENT IN CHINA'S MAINLAND: A SPATIAL STUDY WITH SPECIAL REFERENCE TO THE LOCATIONAL BEHAVIOUR OF INVEST... 相似文献
11.
Based on field investigations, laboratory analyses and 14C dating, this paper discusses the laws of the formation and development of the paleosols in the northeast region of the Qinghai-Xizang
Plateau since Late Pleistocene. The authors reconstruct basic conditions of climate, vegetation, soil and natural zones during
the three periods in which the paleosols were formed, i.e. the last interglacial of the Late Pleistocene, warm stage of Late
Glacial and the Optimum of Holocene. Finally, this paper discusses the relationship between the paleosols and the uplift of
the Qinghai-Xizang Plateau. 相似文献
12.
LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG (TIBET) PLATEAU: A CONTROVERSY TO M. KUHLE,S ICE SHEET HYPOTHESIS 总被引:1,自引:0,他引:1
Since the late 1950's, many Chinese scientists have explored the remains of the Quaternary glaciation in the Qinghai-Xizang (Tibet) Plateau and its surrounding mountains. In the main, 3-4 glaciations have been recognized. The largest one occurred in the Late Middle Pleistocene with piedmont glaciers, ice caps and trellis valley glaciers in many high peak regions. But here is no evidence of a unified ice sheet covering the whole plateau as described by M. Kuhle. Due to the further uplifting of the Himalayas and Qinghai-Xizang Plateau the climate became progressively drier, diminishing the extension of glaciers during the Late Pleistocene. The elevation of the snow line during the Last Glaciation was about 4,000 m on the south, east and northeast edges of the plateau and ascended to 5500 m on the hinder northwest of the plateau. The thermal effect of the big plateau massif, the sharp increase of aridity from the southeast rim to the northwest inland area and the abrupt decrease of precipitation during the 相似文献
13.
Since the late 1950’s, many Chinese scientists have explored the remains of the Quaternary glaciation in the Qinghai-Xizang
(Tibet) Plateau and its surrounding mountains. In the main, 3–4 glaciations have been recognized. The largest one occurred
in the Late Middle Pleistocene with piedmont glaciers, ice caps and trellis valley glaciers in many high peak regions. But
here is no evidence of a unified ice sheet covering the whole plateau as described by M. Kuhle. Due to the further uplifting
of the Himalayas and Qinghai-Xizang Plateau the climate became progressively driver, diminishing the extension of glaciers
during the Late Pleistocene. The elevation of the snow line during the Last Glaciation was about 4,000 m on the south, east
and northeast edges of the plateau and ascended to 5500 m on the hinder northwest of the plateau. The thermal effect of the
big plateau massif, the sharp increase of aridity from the southeast rim to the northwest inland area and the abrupt decrease
of precipitation during the Ice Age largely account for the distribution of the Quaternary glaciers in the Qinghai-Xizang
Plateau. The neglect of Chinese literature may be one of the causes accounting for M. Kuhle’s misinterpretation on the environment
of the Quaternary glaciations in the Qinghai-Xizang Plateau. 相似文献
14.
Wang Jianli 《中国地理科学(英文版)》1997,8(1):85-90
Estimates of the palaeo-subaerial wind direction were studied systematically for the first time by using the anisotropy of
loess magnetic susceptibility (AMS) measurements in the northwestern China. One hundred and forty undisturbed oriented aeolian
loess samples were collected from Lanzhou, Linxia and Wudu areas for AMS measurements, which indicated the subaerial wind
directions were not the same while the loess deposited. From the Early Pleistocene to Middle Pleistocene till Late Pleistocene,
the wind direction experienced an anticlockwise rotation in the studied area. We suggested this change was related to the
uplift of the Qinghai-Xizang Plateau and the adjustment of current and landform effects. 相似文献
15.
太白盆地黄土地层厚16m左右.发育有两层红褐色古土壤。化学分析与微结构鉴定表明该盆地黄土中的古土壤为FeO3与Al2O3迁移深度大但无聚集的棕壤.并已成为明显的风化无,发育时的年平均降水量在1000mm以上.太白盆地黄土中CaCO3含量少,发育有淀积型的光性定向粘土.表明黄土地层发育时的降水量也在600mm以上。该盆地黄土地层发育在距今约20多万年前.指示从这一时期开始,中国黄土搬运高度已超过2000m。微结构的观察还表明,光性定向粘土不仅可用于降水量的研究,也可用于指示温度的相对高低. 相似文献
16.
王建力 《中国地理科学(英文版)》1998,8(1):85-90
THEANISOTROPYOFLOESSMAGNETICSUSCEPTIBILITYINTHENORTHEASTERNFRINGEOFQINGHAIXIZANGPLATEAUASANINDICATOROFPALAEOWINDDIRECTIONWan... 相似文献
17.
Matthias Kuhle 《山地科学学报》2007,4(2):91-124
This overview discusses old and new results as to the controversy on the past glacier extension in High Asia, which has been debated for 35 years now. This paper makes an attempt to come closer to a solution. H.v. Wissmann's interpretation (1959) of a small-scale glaciation contrasts with M. Kuhle's reconstruction (1974) of a large-scale glaciation with a 2.4 million km2 extended Qinghai-Xizang (Tibetan) inland glaciation and a Himalaya-Karakorum icestream network. Both opinions find support but also contradiction in the International and Chinese literature (Academia Sinica). The solution of this question is of supraregional importance because of the subtropical position of the concerned areas. In case of large albedo-intensive ice surfaces, a global cooling would be the energetical consequence and, furthermore, a breakdown of the summer monsoon. The current and interglacial heat-low above the very effective heating panel of the Qinghai-Xizang (Tibetan) Plateau exceeding 4000 m, which gives rise to this monsoon circulation, would be replaced by the cold-high of an inland ice. In addition, the plate-tectonically created Pleistocene history of the uplift of High Asia — should the occasion arise up to beyond the snowline (ELA) —would attain a paleoclimatically great, perhaps global importance. In case of a heavy superimposed ice load, the question would come up as to the glacio-isostatic interruption of this primary uplift. The production of the loesses sedimentated in NE-China and their very probable glacial genesis as well as an eustatic lowering of the sea-level by 5 to 7 m in the maximum case of glaciation are immediately tied up with the question of glaciation we want to discuss. Not the least, the problems of biotopes of the sanctuary-centres of flora and fauna, i.e., interglacial re-settlement, are also dependent on it. On the basis of this Quaternary- geomorphological-glaciological connection, future contributions are requested on the past glaciation, the current and glacial permafrost table and periglacial development, the history of uplift, and the development of Ice Age lakes and loess, but also on the development of vegetation and fauna in High Asia. 相似文献
18.
通过对老灌河河流阶地水平错断幅度和垂直错断幅度的测量 ,证实自晚更新世中期以来黑沟大断裂的构造活动十分强烈 ,主要表现为水平方向上的大规模左旋走滑活动 ,在垂直方向上的活动相对来说比较微弱。不管是水平方向还是垂直方向的活动 ,都表现有加速的趋势。 相似文献
19.
????????-????????жι????ò???????????????????飬???????????????????????????????????????о????????????????棬?????????-????????жι?????λ????????????????????-???????ж???????????????и??????Ъ??????????????м???????,??????????????,??????????????????????ж??????????λ???2~3 km???????????????????????????????γ?????????棻?????????????????NE-NEE??????????????????????????????????????? 相似文献
20.
Zhao Kuiyi 《中国地理科学(英文版)》1997,8(1):44-52
The southern part of the Qinghai-Xizang (Tibet) Plateau and its adjacent area are rich in mire flora. There are 51 families,
101 genera and 220 species. The geographical compositions of this region are very complex, consisting of the following-geographical
elements: tropic-subtropic elements approximating to 8.33% of the entire flora in the region, tropic-temperate elements 22.71%,
temperate elements 43.18%, cosmopolitan elements 9.85%, the Qinghai-Xizang endemic elements 14.39%, north polemountain elements
1.51%. Temperate elements in this region are dominant. The dominant species of mires, Carex lasiocarpa, in this region is also found in northeast China, Finland and North America. The origin of mires of this region is earlier
than northeast China and Finland. This shows that the southern part of the Qinghai-Xizang Plateau and its adjacent areas may
be the centre of the origin and distribution of temperate elements. 相似文献