摘要:In August 1933,I made geological investigations in the vicinity ofBarim station of Chinese Eastern Railway.This area was explored byDr.E.Ahnert in 1901~1,but my explorations were more in detail; I madegeological survey in the scale 1:10,000.All petrological determinations were

摘要:The first geological investigation of the Great Hingan was made inthe year 1901,when Dr.E.Ahnert crossed the northern part of this rangealong the present line of Chinese Eastern Railway.

摘要:Until recently,the geology of the vicinity of Jungcheng city was almostunknown.In the famous work of von Richthofen~1,the whole area of thisregion had not been surveyed at all although the mere district of Cheng-shantou (成山头) has been mapped,erroneously,as a spot of Arch(?)an

摘要:D'après Bailey Willis,~1 le Woutaichan,d'où provient le terme de"Wut'ai System",compose presque entièrement de roches métamorphiques quisont disposées en discordance sur le "T'aishan Complex".Ce dernier cor-

摘要:The occurrences of the Viviparid shells in palaeontic state as well as inrecent form are recorded as abundant from various districts of Yunnan as far asthe old records show.During the later half of the last century,Neumayr,Nevill,Anderson,Mabille,Heude,etc.,the more recently,Dautzenberg,H.

摘要:The map of the Tarim basin and its mountainous border regions rough-ly indicates the distribution of the supposed Eocene sediment and the extensionof the principal mountain ranges and the large general peneplaned old rockregions.It also indicates the principal tectomc units,the interaction of whicl

摘要:The recent discovery of fossil plants in association with fresh-watermollusca,at the type locality of the Sanmenian series at Sanmen Rapids,addsa brief though important chapter to our gradually increasing knowledge of the

摘要:INTRODUCTION Until recent years geologists have tended to lay the greatest emphasis onthe study of the rocks,minerals and fossils of the earth's crust and to pay but littleattention to the soil.Most geologists have taken for granted that the kind of soilin a given region depends largely on the nature of the parent rocks from which the

摘要:INTRODUCTION In the beginning of 1935,a party of geologists was sent by Di.W.H.Wong,Director of the Geological Survey,in order to survey the Cenozoicformations of Kwangsi.The party,including P.Teilhard de Chardin,Dr.C.C.Young and the author,was met in Canton and greatly assisted in thefield by Dr.H.C.Chang,Professor at the Sunyatsen University (Canton).

摘要:The geological observation made in the Kwangsi Caves by P.Teilhardde Chardin,Drs.C.C.Young,H.C.Chang and the author,and the descrip-tion of the cultural remains collected in these caves have been published in twoseparate notes~1.This paper only deals with the description of a small collec-