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1.
A joint meeting of the Geological Society of China, Peking Union Medical College and Peking Society of Natural History was held on October 26 in honour of H. R. H. the Grown Prince ef Sweden. Dr. W. H. Wong presided. The meeting was opened by Dr. H. S. Houghton, the President of the Peking Union Medical College, followed by a welcome address delivered by Dr. W. H. Wong on behalf of the several scientific organizations.  相似文献   

2.
C.C.YOUNG 《地质学报》1944,(Z2):192-214,304,306
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   

3.
A small collection of fossil plants was made in 1930 by Dr.GeorgeB. Barbour,of Yenching University,in the course of his study of the sedimen-tary deposits near Taiku,Shansi Province (See text figure 1).My acknow-ledgement is due to Dr. Barbour,and to Dr. W. H. Wong,Director of the  相似文献   

4.
K. C. YANG 《地质学报》1944,(Z2):176-181
正 The Cambro-Ordovician stratigraphy in the core of the Tapashan, in northeastern Szechuan is dealt with in this paper. The data were collected by the geological excursion party led by Dr. C. Y. Lee, formerly Director of the Geological Survey of Szechuan, in the winter of 1941.  相似文献   

5.
A rich fossiliferous deposit at Chou Kou Tien 70 li to the south west of Peking was first discovered in the summer of 1921 by Dr. J. G. Andersson and later surveyed and partially excavated by Dr. O Zdansky. A preliminary roport on the site was published by Dr. Andersson in March 1923 (Mem. Geol.  相似文献   

6.
王紹文 《地质学报》1932,11(1):71-79
OCCURRENCE. In 1918 Dr. W. H. Wong heard of the occurrence of beryl crystals in Tachingshan, north of Kueihua, from where the crystals were sent to Peiping, but he did not find the exact place of occurrence. Mr. H. T. Chang mentioned in his "Lapidarium Sinicum" that some of the Piyase in the Peiping market is not tourmaline but beryl and, this mineral was said to come from  相似文献   

7.
《地质学报》1932,11(2):101-105
In opening the meeting, the chairman made the following address: "It is my agreable duty to announce and make the award of the Grabau Medal to two members of our Society, Drs. J. S. Lee and Davidson Black. "The Grabau Medal was founded in 1925 by Mr. C. Y. Wang. the then President of the Geological Society. It was so named in honor of Dr. Grabau  相似文献   

8.
9.
In the province of Anhui along the Yangtze River, especially on the south of it there occur many iron deposits. They have been described in "The Iron ore deposits and iron industry of China" by Dr. F. R. Tegengren published by the Geological Survey in the Memoir Series A, No. 2. However Dr.  相似文献   

10.
A small collection of fossil plants was made in 1930 by Dr.GeorgeB. Barbour,of Yenching University,in the course of his study of the sedimen-tary deposits near Taiku,Shansi Province (See text figure 1).My acknow-ledgement is due to Dr. Barbour,and to Dr.  相似文献   

11.
The material dealt with in the present paper was collected by thelate Dr. V. K. Ting in 1933 with the specific object of determining theboundaries of the Carboniferous and Permian developments in Russiaand their stratigraphical relation to the Huanglung, Chuanshan and  相似文献   

12.
The First International Council for Science(ICSU) Regional Meeting for Asia and the Pacific was held from April 25-27, 2005 in Kuala Lumpur, Malaysia. The meeting was hosted by the Ministry of Science, Technology and Innovation of Malaysia and the Academy of Sciences Malaysia. Welcoming remarks were delivered by Tan Sri Datuk Dr. Ahmad Zaharudin Idrus, President,Academy of Sciences Malaysia and Prof. Thomas Rosswall, Executive Director,ICSU. His Excellency Dato‘ Sri Dr. Jamaludin Jarjis, Minister of Science, Technology and Innovation, Malaysia opened the meeting.About 40 participants attended the meeting,representing national science academies from the Asia Pacific and international scientific unions that are active in the region. The International Union of Geological Sciences(IUGS) was represented by the President,Prof. Zhang Hongren. Dr. Joy Pereira, Chair of the IUGS Commission on Geoscience for Environmental Management (IUGS-GEM)also attended the meeting as an Observer.  相似文献   

13.
The present specimen was loaned to me for investigation by my friend, Dr. W. H. Wong, Director of the Geological Survey of China. It was collected from Fan Chuang (范莊) of Si Chuan Hsien (淅川縣), Honan Province by Mr. C. Li (李捷), who conducted a geological surveying trip in  相似文献   

14.
Age of the Kueite Series: In my paper "Essays on the Cenozoic of Northern China" I have mentioned a fossil find which was made by Dr. Wong Wen-hao and Mr. C. Y. Hsieh in the "Red beds" of Ku Yuan Hsien, E. Kansu. These were shells and opercula of a small gastropod which I  相似文献   

15.
李承三 《地质学报》1932,11(1):49-60
Ⅰ. INTRODUCTION In the year 1930, Mr. Taichitao and Dr. Chuchiahua, then President and Vice-President of Sunyatsen University of Canton, were kind enough to offer me a chance to participate on the geological and topographical studies to  相似文献   

16.
In a short paper entitled "Evidences of the Use of Fire by Sinanthropus",Dr.Davidson Black has discussed the occurrence of burned bone fragments andcharcoal debris in association with the remains of Sinanthropus at Chou KouTien,and has concluded that Sina  相似文献   

17.
PY.C.PING 《地质学报》1932,11(1):108-114
Through the courtesy of the Geological Survey of China, I have the previlege of studying the present specimen which was collected by P. Teilhard de Chardin and Dr. C. C. Young of the Survey from Chichiakou (冀家溝) of Pao-  相似文献   

18.
Comprehensive analyses were made based on seismic prospecting data, electrical prospecting data and basin simulation data as well as regional geological data and thorough discussions were conducted about the complicated structures, features and evolution of Hefei Basin in Early Cretaceous in this study, and it was derived that that Hefei Basin was a composite basin formed during the transformation of the stress field from compressive toward tensile in Early Cretaceous. In other words, this basin was a foreland basin of gliding-thrust type, which is mainly controlled by the Dabie orogenic belt in the south side in the early to middle period of Early Cretaceous, while being a strike-slip basin of pull-apart type, which is mainly controlled by the activity of Tanlu fracture in the east side in the middle to late period of Early Cretaceous. Moreover, the potential Lower Cretaceous oil and gas system in the pull-apart basin and the vista for its prospecting were explored in this study. Tectonism of the Tanlu fracture was further discussed based on the results of characterization of the basin, and it was pointed out that this is beneficial and instructive to the oil and gas prospecting in Hefei Basin.  相似文献   

19.
C.C.CHANG  C.Y.JEN 《地质学报》1941,(Z1):202-206
正 The geology along the route from Luting',Tanchang~2,Yungching~5 toYaan~4 was first investigated by H.C.T'an and C.Y.Lee [6].Their resultappeared in the Atlas for "the Geology of Szechuan Province and Eastern  相似文献   

20.
C. J. PENG 《地质学报》1944,(Z1):98-114
正 The discovery of bauxite from a number of places in Kueichou in 1941 made by Dr. S. S. Yoh and his colleagues [13] is of economic as well as scientific significance. In the following year, the writer, in collaboration with Dr. C. Y. Li, had an opportunity of making an investigation of the three de  相似文献   

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