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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1944, 24(Z2):147-165.
Abstract:Since the illuminating study on the Mesozoic stratigraphy of Szechuan by C. Y. Lee [40] and the valuable contributions by T. Y. Hsu [26-32], much light has been thrown upon the Triassic stratigraphy and palaeontology of that region.
1944, 24(Z2):166-175.
Abstract:The occurrence of Triassic strata around the city of Tsunyi~1 in northern Kueichou has been known since the exploration of Yoh in 1927. Two years later, V. K. Ting, T. K. Huang and Y. L. Wang made their journey through Tsunyi and collected some fossils from a series of rocks above the Permian coal
1944, 24(Z2):176-181.
Abstract:The Cambro-Ordovician stratigraphy in the core of the Tapashan, in northeastern Szechuan is dealt with in this paper. The data were collected by the geological excursion party led by Dr. C. Y. Lee, formerly Director of the Geological Survey of Szechuan, in the winter of 1941.
1944, 24(Z2):182-191.
Abstract:The area extending from the Suiyang~2 city in the north to Tuanchi~3 in the south was surveyed by the writers in 1943. Apart from 2 few scattered outcrops of Cenozoic and recent deposits, the major stratigraphical units represented in this area are the Cambrian, the Ordovician, the Silurian, the Permian, and the Triassic systems. Gaps of some importance were observed between the
1944, 24(Z2):192-214,304,306.
Abstract:The following described reptilian remains were unearthed from the vicinity of Weiyuan’ by Mr. H. H. Yao of the National Geological Survey of China when he worked as a member of a geological party under the leadership of Dr. T. K. Huang in 1939. Most of the remains were collected from locality 1 and locality 6, as Yao
1944, 24(Z2):216-220.
Abstract:For many years,there has been considerable difference of opinion in regard to the age of the horizons bearing both Protolepidodendron and Bothriolepis in Central Hunan and Eastern Yunnan.I am in full accord with the view recently put forward by. H. C. Wang that the plant- and fish-bearing series o
1944, 24(Z2):222-224.
Abstract:Among the fossils collected in recent years by the Geological Survey of Kuangtung and Kuangsi is a Sphenophyllum that is of considerable importance for exact confirmation of the presence in south-western Kuangtung of the Wutung Series.The plant-bearing strata are exposed near the village Shachow of the
1944, 24(Z2):226-244.
Abstract:With 5 Plates The region here described as West Hunan includes the drainage area of Yuanshui~1 and Lishui~2 together with their tributaries. As a result of several years' research in this area, the writer has gathered
1944, 24(Z2):245-249,307.
Abstract:Joints are the most prevalent minor fractures in rocks. At first they may give us an impression of being hazardous in arrangement, but careful observation often shows that they really occur according to a certain rule. They are important in tectonic study, because through them the stress-orientati
1944, 24(Z2):250-255.
Abstract:Coal deposits are largely preserved, as is commonly known, in certain structural depressions. In folded regions, coal is usually found in synclinal basins; for the intervening anticlines may already have been eroded away. Within one
1944, 24(Z2):256-270.
Abstract:INTRODUCTION Ⅰ.General Principles Theoretically speaking, under the normal cycle of erosion rivers tend to adjust themselves to structure as the cycle advances and complete adjustment should
1944, 24(Z2):271-273.
Abstract:INTRODUCTION While carrying on geological reconnaissance in the district of Chaochuo~1, SE Sikang in 1943, two localities for producing native copper were noticed by the writer. One is called Wakuolaka~2, situated in the mountainous region to the west of Mekoho~3 valley and lying about 60 km NNE of the Chaochuo city and
1944, 24(Z2):275-282.
Abstract:Ⅰ. INTRODUCTION Close to the grand canyon of the Chingshakiang near Luipo~1 in western Szechuan (Plate I, Fig. 1), there occurs a more or less.flat-topped mountain, which, stretching from the city of Luipo northeastward to Wenshuicheng~2, is
1944, 24(Z2):283-303.
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1944, 24(Z2):293-293.
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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