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1.
《地质学报》1934,(1)
The Special Meeting was held jointly with the Peking Society of Natural History, on May 11, 1934, in the lecture room of the Geological Survey Library, in memory of Dr. Davidson Black who suddenly died of heart failure in his laboratory in Peiping on March 15, 1934 at the age of 49 years. 相似文献
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New Isophlebioid Dragonflies from the Middle Jurassic of Inner Mongolia, China (Insecta: Odonata: Isophlebioptera: Campterophlebiidae) 总被引：2，自引：0，他引：2
Three new species of fossil dragonflies assigned to Sinokaratawia Nel, Huang and Lin in family Campterophlebiidae, i.e.S, daohugouica sp. nov., S. magica sp. nov. and S. gloriosa sp. nov., and new materials of male S. prokopi Nel, Huang and Lin, 2007 are described from the Middle Jurassic of Daohugou, Inner Mongolia, China. An emended diagnosis of genus Sinokaratawia was proposed. 相似文献
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ZHANG Binglan REN Dong 《《地质学报》英文版》2008,(6)
Three new species of fossil dragonflies assigned to Sinokaratawia Nel,Huang and Lin in family Campterophlebildae,i.e.S,daohugouica sp.nov.,S.magica sp.nov.and S.gloriosa sp.nov.,and new materials of male S.prokopi Nel,Huang and Lin,2007 are described from the Middle Jurassic of Daohugou,Inner Mongolia,China.An emended diagnosis of genus Sinokaratawia was proposed. 相似文献
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In 1934,a bone bed was located by the authors of the presentnote in the sandstone immediately overlying the lacustrine limestoneof Yangchi,near Ichang (see Teilhard and Young,1935,fig.1).At thebeginning of 1936 Mr.L.P.Chia of the Cenozoic Laboratory was 相似文献
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The Atlas of Palaeogeography of China was published in 1955. This paper will introduce the impor- tant historical background of the compilation and publishing of the atlas. Actually it was a direct outcome of the famous Main geological structural units of China written by Huang Jiqing in 1945. Confined by the status of geological development of that stage, the atlas mainly presents the variation of the distribution of old landmasses and oceans during different geological stages. The compilation was based on facies types, palaeontological species , and features of regional fauna assemblages . The basic scale of the atlas was 1:1 000 000. There are totally 20 maps, spanning from the Sinian to Triassic of the Mesozoic. The compila-tion was finished in more than three years. The outline of landmasses and oceans, main direction of trans-gression and regression, distribution of fossils, crustal deformation, mineral deposits, as well as volcanic and glacial activities are shown with various patterns and colors 相似文献
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《地质学报》1940,20(1)
The first session of the Fifteenth Annual Meeting of the Geological Societyof China was called to order in the Auditorium of the University of Chungking,Shapingpa, at 9:30 a.m. by President T. K. Huang. Brief introductory remarkswere made by the President, who welcomed all the members of the Societyattending the meeting, especially those who had come from far distant provinces 相似文献
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Gu Yansheng Zhuo Ying Zhang Zejun Faculty of Earth Sciences China University of Geosciences Wuhan 《中国地质大学学报(英文版)》2001,12(1)
INTRODUCTIONVermicular red earth is distributed widely in South China,significant for the research into Quaternary environment andglobal change. Huang (1993) discovered the evidence of human activities-popple tools in vermicular red earth of the middle-upper reaches of Hanshui Riverl Zhu et al. (1991 ) statedthat red earth was a good information carrier of global changeafter the research into tropic red earth and environment byweathered mineral and geochemistry. Zhao and Yang (1995)stud… 相似文献
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950498 Huang Maohuan(Chinese Aeademyof Scienees,Lanzhou Institute of Glaeiologyand Geocryol吃y,Lanzhou,Gansu)A Steady一S扭te Analysis of Iee Tem琳rature tn theGul二ya Iee臼P,West Kunlun Mountains,Chlna(Journal of Glaeiology and Geocryolo--gy,ISSN 1000一0240,CN62一1072/P,19(3),1997,p.202一206,1 graph,12 ref) A borehole,309m in depth,was made at6070m a.5.1.on the Guliya Iee CaP in theWest Kunlun Mountains,of whieh in theu卜most 200m iee temperature was measured.Asteady一state ana… 相似文献
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<正>The Huang Shui River,a main tributary of the Yellow River,crosses a series of tectonically subsided and uplifted areas that show different patterns of terrace formation.The distribution of fluvial terrace of the Huang Shui River is studied through topographic and sedimentologic terrace mapping.Three terraces in the Haiyan Basin,four terraces in the Huangyuan Basin,19 terraces in the Xi'ning Basin(the four high terraces may belong to another river),nine terraces in the Ping'an Basin, five terraces in the Ledu Basin and 12 terraces in the Minhe Basin are recognized.Sedimentology research shows that the geomorphologic and sedimentological pattern of the Huang Shui River,which is located at the margin of Tibet,are different from that of the rivers at other regions.The formation process of the terrace is more complicated at the Huang Shui catchment:both accumulation terrace and erosion terrace were formed in each basin and accumulation terraces were developed in some basins when erosion terraces were formed in other basins,indicating fluvial aggradation may occur in some basins simultaneously with river incision in other basins.A conceptual model of the formation process of these two kinds of fluvial terraces at Huang Shui catchment is brought forward in this paper.First,the equilibrium state of the river is broken because of climatic change and/or tectonic movement,and the river incises in all basins in the whole catchment until reaching a new equilibrium state.Then,the downstream basin subsides quickly and the equilibrium state is broken again,and the river incises at upstream basins while the river accumulates at the subsidence basin quickly until approaching a new equilibrium state again.Finally,the river incises in the whole catchment because of climatic change and/or tectonic movement and the accumulation terrace is formed at the subsidence basin while the erosion terrace is formed at other basins.The existence of the accumulation terrace implied the tectonic subsidence in the sub-basins in Huang Shui catchment.These tectonic subsidence movements gradually developed from the downstream Minhe Basin to the upstream Huangyuan Basin.Dating the terrace sequence has potential to uncover the relationship between the subsidence in the catchment and the regional tectonic at the northeastern Tibetan Plateau. 相似文献
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赵亚曾 《《地质学报》英文版》1929,8(2):139-154
After a period of four months' field work in South Shensi and North Szechuan, Mr. T. K. Huang and I at last arrived, at the end of June, Chengtu where we decided to pass our summer vacation. Shortly after the arrival, Mr. Huang, for some personal affairs, went home in his native 相似文献
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正 With 2 Plates Ⅰ. INTRODUCTION Both Middle and Upper Carboniferous rocks are well developed in Western Kansu and were investigated by Loczy [19], Obrutchev [21],Yuan [31, 32], and Sun [25]. Though the faunas from these rocks have been studied in some detail by Loczy, Chao, Lee and others, their stratigraphic succession and the correlation of fossil horizons found in them in different localities yet remain to be established. In 1941-942, T. K. Huang and party, of which the writer was a member, made reconnaissance 相似文献
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Based on the runoff and meteorological data of Langan(兰干) Hydrological Station from 1957 to 2009 in Keriya(克里雅) River,the periodicities,abrupt changes,and trends of climate factors and runoff were investigated by wavelet analysis and nonparametric test;then,the future change of the annual runoff was predicted by a periodic trend superposition model.In succession,the influencing volumes of climate change on the annual runoff were separated from the observation values of the an-nual runoff in Keriya River.The... 相似文献
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TE-YOU HSU 《地质学报》1937,(Z1)
Early in 1936 Dr. T. K. Huang, Messrs. S. F. Sheng, I. Ting andK. S. Tsui during their field work in the Changhsing coal field, NWChekiang, found Scythic pelecypods and ammonoids in the so-calledChinglung limestone of that region. The discovery of Lower Triassic 相似文献
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982034 Huang HuanDesign Institute of(Urban ArehiteeturalPanyu City,Guangdong)Anvestigatlon andExantple of LOoseTI’e自tment in thePanyu,5011玩- PanyuGuangdong Provinee(Guangdong Ge-ISSN 1 001一8670,CN 44一1201/P,,1 998,P.49一53,with Englisha卜reinforeing bar of diameter 25mm,steel wireand rib一like steel ete.have been sueeessfullyapplied in the engineering eonstruetion ofm闭ern bridges.982035 Huang Yahong(Lanzhou Institute ofSeismology,CSB,Lanzhou,Gansu)TheAnalysis and Predieti… 相似文献
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Y. WANG Geological Survey of China 《地质学报》1944,(Z2):166-175
正 The occurrence of Triassic strata around the city of Tsunyi~1 in northern Kueichou has been known since the exploration of Yoh in 1927. Two years later, V. K. Ting, T. K. Huang and Y. L. Wang made their journey through Tsunyi and collected some fossils from a series of rocks above the Permian coal 相似文献
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<正>20152023 Cai Baoxin(Yunnan Institute of Geological Environmental Monitoring,Kunming650216,China);Huang Yu An Analysis of Differences in Accumulation of Heavy Metals in Main Crops in a Tin Mining Area of Yunnan Province(Geological Bulletin of China, 相似文献
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Since the publication, in June 1933, of "Fossil Man in China", up to the present date (September 1934), a series of new observations have been made in the course of the Chonkoutien excavations. Although these new 相似文献
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The following described reptilian remains were unearthed from the vicinity of Weiyuan’ by Mr. H. H. Yao of the National Geological Survey of China when he worked as a member of a geological party under the leadership of Dr. T. K. Huang in 1939. Most of the remains were collected from locality 1 and locality 6, as Yao 相似文献