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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1934, 13(0).
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1934, 13(0).
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1934, 13(0).
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1934, 13(0).
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1934, 13(0).
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1934, 13(0).
Abstract:Eleven years ago when this society held its Third General Meeting I had the opportunity of calling your attention to certain strange deposits and topographical features that came under my notice in certain parts of North China. I showed you a number of st
1934, 13(0).
Abstract:Bordered by the Chungtiaoshan (中條山) on the North and the Tsinling (秦嶺) on the South, the area between Loyang and Sian, where the Huangho River hits and follows the old Weiho valley has been known for a long time to be specially rich in Cenozoic formations
1934, 13(0).
Abstract:GENERAL FEATURES. The Upper Yangtze valley includes the valleys of the main river and its chief tributaries. Chinshactiang (金沙江) and Yalungchiang (雅龍江) flow in north-south courses through Hsikang, Eastern Tibet, and turn to NEE
1934, 13(0).
Abstract:INTRODUCTION During the year 1930-31, while holding a schularship from the Harvard-Yenching Institute, I received permission from the Institute to engage in ethnological and anthropological research on behalf of the University Museum
BORIS LICHAREW , LENINGRAD USSR~
1934, 13(0).
Abstract:The study of the Upper Carboniferous has been attracting much attention recently and the question as to its extent and stratigraphy has been the object of very serious discussion, but so far without any positive results. The large territory of the Soviet
1934, 13(0).
Abstract:INTRODUCTION One of the major structural features in north China is the great fault system in central Shensi and Shansi known as the Weiho (渭河) Graben and Fenho (汾河) Craben respectively (Fig. 1). Dr. Bailey Willis seems to
1934, 13(0).
Abstract:Maping, formerly named Liuchow, is one of the well known cities in Central Kwangsi. The geology of the Maping district and its neighbouring areas were preliminarily surveyed by S. S. Yoh in 1929. In our journey across the Nanling Range we passed through t
1934, 13(0).
Abstract:Meitien is one of the largest villages in Ichanghsien, Hunan, and is situated about 20 km. west-southwest of the Ichang City. The well-known Chitienling (騎田嶺), one of the "Five Ranges" of the Nanling, stands on the north side of Meitien, at a distance of
1934, 13(0).
Abstract:INTRODUCTION The specimens described in this paper were collected by Mr. Y. Y. Lee from the Meitien Limestone, Meitien, Ichang South Hunan. According to Mr. Lee this limestone occurs in isolated outcrops overlying the Lungtan
C. S. KAO Y. H. HSIUNG & P. KAO
1934, 13(0).
Abstract:CONTENTSIntroduction Description of sections Chihsien (薊縣) and Hsinglunghsien (興隆縣), Hopei
1934, 13(0).
Abstract:INTRODUCTION Shuikoushan is the most important and well known mining district for production of silver, lead, zinc and pyrite in China. It is situated at about 65 li N. E. of Changning, 90 li S. of Hengyang and 620 li from Changsha, the Capital of Hunan.
BY W. C. PEI Cenozoic Research Laboratory , Geological Survey of China
1934, 13(0).
Abstract:1. INTRODUCTION When inspecting the Choukoutien area in October 1933, under the direction of the late Dr. Davidson Black, the workmen brought to the attention of the members of the Cenozoic Laboratory a fossiliferous site which had
1934, 13(0).
Abstract:The presence of Dicynodontia in Sinkiang was first made manifest by the beautiful skull described in the same number of the Bulletin, (see above 563) as Dicynodon sinkianensis sp. nov. Recently, a second skull also collected by
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1934, 13(0):82--100.
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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