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1.
WANG Xueqin WANG Tao JIANG Jin & ZHAO Congju . Laboratory of Blown Sand Physics Desert Environment Cold Arid Regions of Environmental Engineering Research In-stitute Chinese Academy of Sciences Lanzhou China . Xinjiang Institute of Ecology Geography Chinese Academy of Sciences Urmqi China Correspondence should be addressed to Wang Xueqin 《中国科学D辑(英文版)》2005,(6)
Longitudinal dunes,also known as linear dunes,are the most widespread of all dune types,which occupy1/2to2/3of the total area in the world sand seas.They mainly occur in the southern part of Africa,Arabian Peninsular,Australia,Central Asia and North Af-rica-Middle East regions[1],in China they mainly ap-pear in the Gurbantnggt Desert.Many researches have been done on wind dynamics of the sand dune and its relations with environmental conditions[2—9],but comprehensive studies on sand … 相似文献
2.
GUO AnLin? ZHANG GuoWei SUN YanGui ZHENG JianKang LIU Ye & WANG JianQi National Key Lab of Continental Dynamics Northwest University Xi’an China Qinghai Institute of Geological Survey Xining China 《中国科学D辑(英文版)》2007,(2)
The mafic volcanic association is made up of OIB, E-MORB and N-MORB in the A'nyemaqen Paleozoic ophiolites. Compared with the same type rocks in the world, the mafic rocks generally display lower Nb/U and Ce/Pb ratios and some have Nb depletion and Pb enrichment. The OIB are LREE-enriched with (La/Yb)N =5―20, N-MORB are LREE-depleted with (La/Yb)N = 0.41―0.5. The OIB are featured by incompatible element enrichment and the N-MORB are obviously depleted with some metasomatic ef- fect, and E-MORB are geochemically intermediated. These rocks are distributed around the Majixue- shan OIB and gabbros in a thickness greater than a thousand meters and transitionally change along the ophiolite extension in a west-east direction, showing a symmetric distribution pattern as centered by the Majixueshan OIB, that is, from N-MORB, OIB and E-MORB association in the Dur'ngoi area to OIB in the Majixueshan area and then to N-MORB, OIB and E-MORB assemblage again in the Buqing- shan area. By consideration of the rock association, the rock spatial distribution and the thickness of the mafic rocks in the Majixueshan, coupled with the metasomatic relationship between the OIB and MORB sources, it can be argued that the Majixueshan probably corresponds to an ancient hotspot or an ocean island formed by mantle plume on the A'nyemaqeh ocean ridge, that is the ridge-centered hotspot, tectonically similar to the present-day Iceland hotspot. 相似文献
3.
LIU ZhiQiang LAI YuanMing ZHANG MingYi & ZHANG XueFu State Key Laboratory of Frozen Soil Engineering Cold Arid Regions Environmental Engineering Research Institute Chi- nese Academy of Sciences Lanzhou China School of Civil Engineering Lanzhou Jiao Tong University Lanzhou China Chongqing Jiao Tong University Chongqing China 《中国科学D辑(英文版)》2007,50(3):404-410
The stochastic finite element equations for random temperature are obtained using the first-order per-turbation technique taking into account the random thermal properties and boundary condition, based on heat transfer variational principle. The local average method for 2-D is used to discretize random fields. Then, the random temperature fields of embankment in cold regions are investigated on condi-tion that the thermal properties and boundary condition are taken as random fields, respectively, by using the program, which is written by the methods. The expected value of temperature field and the standard deviation of the temperature field of embankment in cold regions are obtained and analyzed. 相似文献
4.
ZHOU Gangyan ZOU Jiazhong 《国际泥沙研究》1997,(1)
I.m~UCrIONBedloadisthesedimentwhichmovesalongtheriverbedintheformofrolling,slidingandsaltation.BedloadmaycreatemanyproblemsintheoperationandmaintenanceofnavigationchannelandinthedevelOPmentofhydroelectricity.Dataofbedloaddischargearealsorequiredinthedesignofreservoir,inwhichtheinflowbedloadareallactuallytrapped.Thewaysofbedloadmotionaredifferentfordifferentsizes.Thus,itisextremelydifficulttodeterminethebedloaddischargeaccurately.Manyequationshavebeenproposedtocalculatethebedloaddischarge.H… 相似文献
5.
Nikki White Eduardo Garzanti Malcolm Pringle Randy Parrish Geoff Nowell Yani Najman Mike Bickle Peter Friend Hazel Chapman Doug Burbank Ashok Maithani WT ”BX 《地学前缘》2000,(Z1)
THE PROVENANCE OF THE DHARAMSALA FORMATION1 NajmanY ,GarzantiE .ReconstructingearlyHimalayantectonicevolutionandpaleogeographyfromTertiaryforelandbasinsediments,NorthernIndia[J].GSABulletin ,2 0 0 0 .inpress
2 OliverGJH ,JohnsonMRW ,FallickAE .AgeofmetamorphismintheLesserHimalayaandthemainCentralThrustzone ,GarhwalIndia :resultsofillitecrystallinity ,4 0 Ar 3 9ArfusionandK Arstudies[J].GeolMag 1995 ,132 (2 ) :139~149.
3 PognanteU ,CastelliD ,BennaP ,eta… 相似文献
6.
Co-seismic ground deformation and source parameters of Mani M7.9 earthquake inferred from spaceborne D-InSAR observation data 总被引:4,自引:0,他引:4
SHAN Xinjian MA Jin WANG Changlin LIU Jiahang SONG Xiaoyu & ZHANG Guifang .Institute of Geology Laboratory of Tectonophysics China Seismological Bureau Beijing China .Institute of Remote Sensing Application Chinese Academy of Sciences Beijing China 《中国科学D辑(英文版)》2004,47(6):481-488
In recent ten years, Differential Interferometric Synthetic Aperture Radar (D-InSAR) has become a major technique of space-based geodesy together with GPS, VLBI and SLR. Interferometric Synthetic Aper-ture Radar (InSAR) has many advantages, such as all-weather, all-time, strong stability and dynamic survey property, and no requirements for ground sta-tions. In particular, the surveying results by InSAR can cover a large range of the ground deformation field in succession and has gr… 相似文献
7.
Transition from platemargin to intraplate environment: Geochemistry of basalts in Paleogene Liaohe basin,northeastern China 总被引:3,自引:0,他引:3
WU Changzhi GU Lianxing REN Zuowei ZHANG Zunzhong CHEN Zhenyan & ZHAO Ming . State Key Laboratory of Mineral Deposit Research 《中国科学D辑(英文版)》2005,48(12):2069-2080
Mesozoic and Cenozoic volcanic rocks are widely distributed in the circum-Pacific area of eastern China. These rocks have long been genetically linked to westward subduction of the paleo-Pacific oceanic plate to the eastern Asia continent[1,2]. Research in re-cent years[3―6] has attained conclusions that a simple paleo-Pacific subduction model does not work well in interpreting all the volcanic rocks in eastern China, although some of them could be attributed to circum-Pacific interaction … 相似文献
8.
ChinaisoneOfthecountrieswhichsufferfromthemostserioussoilerosionintheworld,andthehillyandgullyareasof~PlateauinthemiddlereachesOftheYellowRiverarethemostseriouserosionareainChina.Inthisarea,themainerosivefactorsarerainfallandrunoff.Sometimes,thesedimentyieldinasinglefloodeventcanbe40%oftheannualsedimentload.Therefore,itisveryimPOrtanttostudytheyieldandgraphOfSedimentOfsinglefindevent.Forthispn~,thispaperiswritten.AInongsedimentmodelsforsinglefloodevent,moreandmoreattentionwaspaidtOunitse… 相似文献
9.
10.
TECTONO-SEDIMENTARY EVOLUTION OF THE TERTIARY BASINS IN EASTERN TIBET: CONSTRAINING THE RAISING OF TIBETAN PLATEAU1 YinA ,HarrisonTM .TheTectonicEvolutionofAsia[M] ..Cambridge :CambridgeUniversityPress,1996 .4 4 2~ 4 85.
2 SunH ,ZhengD .FormationevolutionanddevelopmentofTibetanPlateau[M ] .Guangzhou :GuangdongScienceandTechnologyPress,1998.73~ 2 30 .
3 ShiY ,LiJ,LiB .UpliftandEnvironmentalChangesofTibetanPlateauintheLateCen… 相似文献