On the Unconformity between the Triassic and Jurassic in Weiyuan, Szechuan     

T.K.HUANA  H.H.YAO Geological Survey of China 《地质学报》1940,(Z1)

To the north of the famous Tseliutsing salt district of central Szechuanthere exists a big dome-anticline, which is clearly shown in Tan and Lee's [1]Atlas for "Geology of Szechuan and Sikang." Since this anticline occupies thegreater part of the district of Weiyuan, it may be conveniently termed the  相似文献   

On the Possible Oil Fields in Szechuan as Indicated by Isocarb Lines     

Y.HCHIN  V.C.IUAN 《地质学报》1940,(Z1)

Ⅰ. INTRODUCTION From the considerations of the scattered oil occurrences and suitablegeological structures, the Red Basin of Szechuan has long been regarded as apromising country for oil prospecting. In the last decade much attention hasbeen paid by geologists and engineers to the search for oil resources in certain  相似文献   

An Outline of the Geological Structure of the Western Hills of Peiping     

C.Y.HSIEH 《地质学报》1937,(Z1)

As a pioneer worker in almost every phase of the Chinese geology,the late Dr. V. K. Ting was also a pioneer and enthusiastic worker inthe geology of the Western Hills. It was due to his noble effort andsupervision that the first systematic investigation of 1916 was carried out  相似文献   

Fundamental Concepts in Geology and Their Bearing on Chinese Stratigraphy     

A.W.GRABAU 《地质学报》1937,(Z1)

Students of Geology are today confronted with the necessity of anew attitude, which they have to take towards a number of fundamentalgeological concepts which have arisen within the last decade or two.  相似文献   

Contribution to the Marine Lower Triassic Fauna of Southern China     

TE-YOU HSU 《地质学报》1937,(Z1)

Early in 1936 Dr. T. K. Huang, Messrs. S. F. Sheng, I. Ting andK. S. Tsui during their field work in the Changhsing coal field, NWChekiang, found Scythic pelecypods and ammonoids in the so-calledChinglung limestone of that region. The discovery of Lower Triassic  相似文献   

STRATIGRAPHY OF SOUTHEASTERN HUPEI     

谢家榮 《地质学报》1924,3(2)

The geology, of the southeastern part or Hupei has been studied by Mr. Seijirro Noda of the Japanese Geographical Society in 1912. A geological map in the scale of 1:400,000 was prepared by him, covering the districts Ta Yeh, Yang Sing, O Cheng and Wu Chang. Mr. Noda classified the sedimentary rocks into the following series:  相似文献   

L''■GE DU MARBRE DE FANG CHAN ET SA TENEUR EN MAGNESIE     

W.H.WONG 《地质学报》1924,3(2)

Le beau marbre qui entre dans une si grande proportion dans la construction des palais et des monuments a Peking vient d'une region situee a 60 kilometres environ (a vol d'oiseau) au sud-ouest de la Capitable. C'est une partie du plateau qui borde immediatement la plaine alluviable qu'on  相似文献   

ON THE OCCURRENCE OF SPHAEROSIDERITE IN A SUBBITUMINOUS COAL FROM HSIAN COAL MINE,LIAONING PROVINCE     

謝家榮 《地质学报》1933,(1)

Mr.T.F.Hou,geologist of the National Geological Survey of Chinabrought back in 1931 from Liaoning province,a specimen of subbituminous coalin which are included patches or aggregates of small oolites.This interestingspecimen was given to the writer for microscopical investigation.Both polished  相似文献   

ON THE OCCURRENCE OF LYTTONIA FAUNA IN THE VICINITY OF KWEI-YANG,KWEI-CHOW PROVINCE     

乐森璕 《地质学报》1927,6(1):51-52

The so-called Lyttonia Fauna in its broader sense, is known at presentto have an universally wide geographical distribution. It had been reportedoccurring in Texas and Canada of North America; Palermo of Mediterranean  相似文献   

SOME NOTES ON THE CONTACT BETWEEN THE YANGFANG GRANITE AND THE OVERLYING TIAO-CHI-SHAN BEDS.     

朱森  黄汲清 《地质学报》1928,(Z1)

Early in July, 1928, Mr. H. K. Lin, the noted lawyer of Peking, approached Dr. W. H. Wong, director of the Geological Survey of China, for solution of some water supply problems, recently arisen in a tract of hilly land (of which Mr. Lin is the owner) in the eastern foot of the Mont Miao FengShan  相似文献