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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1936, 15(1):17-21.
Abstract:In the lamented death of Dr.V.K.Ting on January 5th,1936,atthe age of 49,China suffered an irredeemable loss.He may be called thefounder of the science of geology in China,and it was in geological field workthat his contribution was especially great.After his graduation from the Uni-versity of Glasgow he made his way back from Europe to China in 1912 by
1936, 15(1):23-51.
Abstract:The Chronological classification of the rocks of the Earth's crust beganin the 18th century when John Strachey in England,Giovanni Arduino inItaly and Lehman,Füchsel,and Werner in Germany began their subdivisionon the lithological and structural basis.
1936, 15(1):53-60.
Abstract:One leading fact that distinguishes the Mesozoic from the Pal(?)ozoic Erain China is the great contrast in wide extent of lands and the withdrawal of theepicontinental seas from the Chinese basins.Such a change might be theoreti-
1936, 15(1):61-74.
Abstract:INTRODUCTION That there are close relations between Orogenesis,Vulkanism andformation of metallic deposits is unanimously accepted by geologists.Amongthe different metallogenetic epochs in China,the late Mesozoic and earlyTertiary periods seems to have given the most important and at the same timethe most varied metallization.It is remarkable to see that it is also during
1936, 15(1):75-85.
Abstract:In the spring of 1934,Mr.T.F.Hou and the writer were instructed bythe Geological Survey of China to explore the provinces of Kansu~1 and Ninghsiawith a view to extending the geological map~2 of Suiyuan.They left Peiping onthe 7th of May and arrived in Kansu on the 19th.A few days later they
1936, 15(1):87-104.
Abstract:INTRODUCTION The maganese deposit of Hsihutsun was first visited by Dr.V.K.Ting~1 in 1922.During the spring of 1932 while directing students of the Geolo-gical Department of the Peking University in the field,the writer had an op-portunity to study the deposit.A detailed geologic map has been prepared,but
1936, 15(1):105-108.
Abstract:For a long time I have been doubtful of the age of a nearly homogeneousgroup of greenish shales which was repeatedly found to lie below the NingkouShale,a graptolite-bearing shale of Arenigian age,so familiar and widely dis-tributed in N.Kiangsi,S.Anhui and S.W.Chekiang.Wherever we metthe Ningkuo Shale in these provinces ,we met the underlying greenish shalestoo.
1936, 15(1):109-114.
Abstract:Anfangs 1934 zeigte Dr.Y.C.Sun dem Verfasser einen Knorriα-(α|¨)hnlichen Sfammrest (Taf.2,Fig.7),den er als Psilophyton dachte.Der Stammwurde in den mittel-devonischen Schichten aus dem Fundort Tiaomachien etwa
1936, 15(1):119-129.
Abstract:It is quite generally accepted that the growth of the Pleistocene ice-capsdemanded world-wide depression of mean sea-level; indeed,as Henri Bauligsays,"it expresses a physical necessity." There is striking evidence,moreover,for such a recent depression in the extension of river systems across the continental
1936, 15(1):131-134.
Abstract:In 1919,while on a visit to Wuning,Kiangsi,I happened to cross arock exposure along the northern slope of Shuangchiaoshan (双桥山) 1 mileand half SSE,of Honlu (横路).My attention was immediately attracted bythe presence of a peculiar bed,which consists of a fine,gray clay mixed upwith sands of various sizes and sub-angular pebbles and which has a thicknessof about 5 m.~2
1936, 15(1):1900/1/1 0:00:00-16.
Abstract:Opening the first meeting at 9:30,the chairman remarked that he wasexceedingly glad to notice the presence of more than 70 members some of whomcame from far distant provinces.This was all the more remarkable at a timewhen the general situation in China is so discouraging.Then he opened thememorial service for Dr.V.K.Ting who died on January 5th at Changsha as
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