UPPER PALAEOZOIC FORMATIONS AND FAUNAS OF YAOLING,CHENHSIEN,S.HUNAN.

STRATIGRAPHY Yao Ling (瑤林) lies 40 li southeast from Chen Hsien city (郴縣), about Long. 112°30′E., Lat. 25°40′N., and is halfway between Chen Hsien city and the well known wolfram mining district, Yao Kang Sien (瑤崗仙). On the     

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     

GEOLOGY OF KENKOU ON THE HUNAN-KWANGTUNG BORDER AND ITS BEARING TO THE OROGENY OF THE NANLING RANGES

INTRODUCTION In the winter of 1932 and the spring of 1933, the Nanling Mountain ranges covering the borders of Hunan, Kwangtung, Kwangsi and Kueichou were studied by the members of the National Research Institute of Geology,     

NOTE ON THE STRATIGRAPHY OF THE ENVIRONS OF THE MAPING CITY, CENTRAL KWANGSI

Maping, formerly named Liuchow, is one of the well known cities in Central Kwangsi. The geology of the Maping district and its neighbouring areas were preliminarily surveyed by S. S. Yoh in 1929. In our journey across the Nanling Range we passed through t     

NOTE ON A PHASE OF THE HERCYNIAN MOVEMENT IN SOUTHERN ANHUEI.

The Hercynian Movement is a well known and almost world-wide orogenetic movement. It embraces all the movements which took place in between the time limits of the beginning of the Carboniferous and the end of the Permian. In China the Kuenlun and Tsinling Ranges are generally supposed to have     

ON A TETRAPORA IN THE LOWER CARBONIFEROUS ROCK OF SOUTHERN HUNAN

INTRODUCTION In the course of his journey across the Nanling range the writer observed two specimens of the present form (Tetrapora carbonica sp. nov.) embedded in a dense blackish gray limestone. Unfortunately the limestone is so dense that     

利用InSAR研究乌恰地震同震形变

2008年10月5日在新疆乌恰地区39.50°N、73.64°E处发生MW6.7地震,用ROI_PAC软件处理4景日本ALOS卫星数据得到乌恰地震的三维同震形变场。距离向,断层北侧最大位移达39 cm,南侧最大位移达36 cm;方位向,北侧和南侧的最大位移分别为1.5 m和2 m。采用Okada弹性位错模型分析该地震的滑动分布,模拟得出的断层走滑角为48°,倾滑角为53°,深度为10.5 km,最大形变量2.5 m,分析得出该地震为向北逆冲兼左旋走滑。     

NOTE ON THE STRATIGRAPHY OF THE ENVIRONS OF THE MAPING CITY, CENTRAL KWANGSI

Maping, formerly named Liuchow, is one of the well known cities in Central Kwangsi. The geology of the Maping district and its neighbouring areas were preliminarily surveyed by S. S. Yoh in 1929. In our journey across the Nanling Range we passed through that city, and had a chance to make a reconnaisance (Feb. 18-22, 1933) in the environs. Here we were     

嘉陵江觀音峽及天府煤鑛區之地質觀察

二十八年三月上旬乘假期數日,率中央大學及重慶大學學生,作嘉陵江三峽區地質實習之行。旅中最後三日駐足於觀音峽及天府鑛區,除普通觀察外并略作地質問題之追尋。所得結果,似有數點爲前人所未詳言,茲簡述之以供討論: