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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1923, 2(Z1):1-16.
Abstract:Morning Session of Saturday, January 7.President H.
1923, 2(Z1):17-27.
Abstract:In my work, Lapidarium Sinicum, the chapter on brass is speciallydevoted to this inquiry. Recently Dr. Read of the U. S. Bureau of Mineswrote to Dr. Ting, suggesting the question whether "The knowledge ofzinc-smelting in India is previous to that developed in China." Therefore
1923, 2(Z1):29-33.
Abstract:INTRODUCTION. I was appointed to accompany Dr. J. G. Andersson to take a trip incentral Shantung. especially in Men Yin (蒙阴) and Lai Wu (莱芜),valleys,for the purpose of collecting fossils and observing the post-Palaeozoic forma-tions. We came back to Peking in December, 1922. The conclusion
1923, 2(Z1):35-78.
Abstract:Ⅰ. INTRODUCTION. "One of the striking features in the Tsinan plain is a group ofisolated hillocks standing up boldly from it. Though mainly overgrown withvegetation, they are distinguishable by ther shape and dark colour from thelight-grey tabular limestone islands which for the last outposts pushedforward by the mountains lying to the south."
1923, 2(Z1):79-91.
Abstract:In regard to the knowledge of the constitutions of coal we are still inthe Dark Ages. To the man in the street, coal is merely a dirty mass ofcombustible matter; to the engineer it is generally thought of in termsof its contents in carbon, velatile matter, moisture, ash and sulphur;
1923, 2(Z1):93-100.
Abstract:The Cambrian of China is developed in Yunnan, Shantung, Chihliand Manchuria. The first collection of Cambrian fossils was made by VonRichthofen and described by Dames and Kayser. Dames studied thetrilobites and Kayser described the brachiopods.
1923, 2(Z1):101-104.
Abstract:INTRODUCTION. The upper Cambrian of Fengtien was studied by Dr. Andersson whomade the following section and kindly permitted me to use it. (Fig. 1) Theupper Cambrian rest disconformably upon the pre-Cambrian rocks, which areof Sinian age. Upwards it is succeeded probably with a disconformity bythe Ordovician.
1923, 2(Z1):105-109.
Abstract:INTRODUCTION The Sinian rocks in China as far as we know are most well developedin Chihli and Shansi provinces. In Chihli, they are usually restricted to theupper part, as in Ta Yang, Pei Yu, Hsia Ma Ling, Ching Pei Kou and other
1923, 2(Z1):111-115.
Abstract:The structure of Nankou is characterized by large and small folds.might faults and abundant igneous intrusions in the form of dikes and sills.Anticline of considerable magnitude extends east and west with a squenceof siliceous limestones and alternating beds of slates and quartzites forming
1923, 2(Z1):117-119.
Abstract:Mr. H. C. T'an (谭锡畴), geologist to the National Geological Surveyof China, during a recent trip (March-May, 1923) through eastern Shan-tung has made an immense collection of fossile from the Jurassic andEocene rod beds. Of special interest are the fossil insects, reptiles, and
1923, 2(Z1):121-123.
Abstract:
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