Chief Editor:HOU Zengqian
Governing Body:China Association for Science and Technology
Organizer:Geological Society of China
start publication :1922
ISSN:ISSN 1000-9515
CN:CN 11-2001/P
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1924, 3(1):1-19.
Abstract:Morning Session of Saturday, January 5. President V. K. Ting in the Chair. The first session of the Second Annual Meeting was called to order at 10 o'clock a. m., Saturday, January 5 in the Library Building of the National Geological Survey of China, Peking, by President Dr, V. K. Ting.
1924, 3(1):21-26.
Abstract:西湖在杭州城西,故名。唐宋以後,為名人遊眺歌詠之地,故其名愈著。汉時曰明聖湖,見水经注。(水經注卷四十云,縣南江侧有明聖湖,父老傅言湖有金牛,古見之神化不测,湖取名焉。顧祖禹方輿纪要謂汉時金牛見湖中當本此。) 又称錢唐湖,以介於錢
1924, 3(1):26-29.
Abstract:Hsi Hu, the Western Lake of Hanchow, has been famous as summer resort and playing ground since the Tang and Sung Dynasties. During the time of Han, however, it was called Ming Shen Hu (明聖湖) while in the time of three Kingdom, it was called Chien Tang Hu (錢塘湖), the latter name being derived from the river, Chien Tang Kiang. Since the Hanchow city was built in the Sui Dynasty which is several hundred years after Han. so the history of Hsi Hu should be reckoned as much older than the city itself. On the other hand, Hsi Hu has never been noticed in any writings before the time when Shiuchinchu (水經註) was published.
1924, 3(1):31-36.
Abstract:Ⅰ. Introduction Our knowledge concerning the geological and geographical ranges of the genus Gigantopteris was summarized by Prof. H. Yabe in one of his papers published in the year 1917, in which Mr. K. Koiwai described three
TEILHARD DE CHARDIN AND F. LICENT.
1924, 3(1):37-44.
Abstract:During the last summer (1923), the authors of this paper were sent by the National Museum of Paris and by the French Ministere de l'Instruction publique for a geological mission in Inner Mongolia. Leaving from Pao T'eou, the geologists crossed the Oula Shan, took a view of the Scheiten Oula
TEILHARD DE CHADIN AND F. LICENT
1924, 3(1):45-50.
Abstract:During the journey in Inner Mongolia, the geological results of which we have summarized in the preceding communication, we had the good fortune, F. Licent and I, of finding, in three different places (along the Choei Tong K'eou in the South of Ning Hia, along the Sjara Osso Gol in the southeastern corner of the Ordos, and near the village of You Fang T'eou in the South of Yu Lin), palaeolithic remains, in excellent stratigraphical and palaeontological conditions.
J.S.LEE The Geology Department of The National University , Peking.
1924, 3(1):51-54.
Abstract:Little doubt can exist regarding the close affinity between Fusulina (MOLLER) and Schwagerina (MOLLER), though there is much room for discussion as to their genetic relation. The recognized affinity seems to depend rather on their common departure from other members of the family, for
1924, 3(1):55-71.
Abstract:The Algonkian sediments of western Shansi are represented by a sedimentary and eruptive formation of very great thickness. They consist of coarse and fine groined sandstones, generally of reddish brown and white colour, interbedded with inconsistent coarser and finer conglomerate layers and reddish brown shales. The formation is intruded by diabases, occuring partly as vertical or oblique dikes, and partly as intrusive or effusive sheets.
1924, 3(1):73-84.
Abstract:Dans un recent travail, publie par le "Bulletin of the Geological Society of China" le Professeur A. W. Grabau a propose de conserver dans la nomenclature stratigraphique de la Chine le terme "Systeme Sinien", autrefois cree par Richthofen, mais en limitant son extension aux couches homologues du systeme local de Hu To (Neo-Pr(?)terozoique), tel qu'il fut defini par Bailey Willis.
1924, 3(1):85-89.
Abstract:In the territory leased to Great Britain, which lies to the South of the Sam Chun river, there are many small areas of sedimentary rocks. A series of red beds, a calcite-bearing conglomerate and a calcite-bearing
Chief Editor:HOU Zengqian
Governing Body:China Association for Science and Technology
Organizer:Geological Society of China
start publication :1922
ISSN:ISSN 1000-9515
CN:CN 11-2001/P