STRATIGRAPHY OF SOUTHEASTERN HUPEI

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:     

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

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     

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

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     

BRIEF NOTE ON REDDISH BROWN SANDSTONE FORMA TION AND TERRACE DEPOSIT IN NORTHERN SOUTH MANCHURIA

As regards to the geological features of the vast area in the northernSouth Manchuria which extends from the north of Kaiyuan(开原) to theneighbouring districts of Harbin, no detailed survey report has yet been     

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

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     

ON THE OCCURRENCE OF LYSTROSAURUS IN SINKIANG~1

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     

察尔汗盐湖察尔汗二级补给系统S3盐层晶间卤水中KCl的分异特征、富集规律及其成因

据ＫＣｌ含量的概率分布特征,晶间卤水分为７个总体。晶间卤水ＫＣｌ,在三级系统内水平分异有２种、剖面分异有５种,二级系统内水平分异呈环带状、剖面分异形式为三级系统内分异形式的组合,垂直分异有１３种;富集的总体为Ⅳ（ｋｃｌ）、Ⅲ（ｋｃｌ）用Ｖ（ｋｃｌ）、三级系统为（８）和（１０）号、部位为固相钾高含处;分异及富集的成因主要为晶间卤水的阶段性淡化。