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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1947, 27(0):1-26.
Abstract:Professor Grabau was one of the most eminent American palaeontologists and geologists of this century. The biographical note of him was written by late V. K. Ting in Grabau's 60th Anniversary Volume of the Geological Society. The present note is to give more details regarding his work and life during the recent 15 years. He was born in Wisconsin in 1870. He studied first in the
1947, 27(0):27-29.
Abstract:It was with pain and grieved emotion that I received the news of Professor Amadeus Grabau's decease some time ago; and I felt, deeply and warmly, that I had lost a real and faithful friend, one who had been close to me in bright and gloomy periods for very many years. Around his bier were assembled in sorrow
1947, 27(0):31-34.
Abstract:Amadeus William Grabau was born of German stock at Cedarburgh, Wisconsin, January 9, 1870. His grandfather was a protestant Lutheran clergyman and so was his father. At the age of fifteen he was apprenticed to a book-binder in Boston. He received his professional grounding as a geologist and palaeontologist in the Boston Society of Natural History (1890), the Massachusetts Institute
1947, 27(0):35-54.
Abstract:The present paper is the outcome of an attempt to answer the problem of glaciation of the Kweichow Plateau raised some six years ago (1). In a region where essentially similar physiographical conditions now prevail, and presumably have prevailed at any given epoch in recent geological times, we ar
1947, 27(0):55-83,413,414.
Abstract:During recent years the geology of Szechuan is becoming better known through the studies of the Geological Survey of China and the Geological Survey of Szechuan. In regard to oil geology and the geology of salt, we are especially indebted to the works of Mr. Y. Y. Lee of the Yungli Chemical Indust
1947, 27(0):85-92.
Abstract:Shansi province covers the mountainous territory W. and S.W. of Peiping and its capital Taiyuan is situated approximately in the centre of the province and at a distance of about 400 km. in a southwestern direction from the old capital. In the 20's and 30's numerous areas of highly alkaline rocks were discovered in Shansi by the Geological Survey of China and the Sino-Swedish Research
1947, 27(0):93-97,99,100,415.
Abstract:The genus Cardiograptus was first figured by Harris in 1916 and described by the same author in 1924 (1). He later studied in great details the phylogeny of Isograptus caduceus and i(?)s allies in Victoria (2). He was inclined to believe that Oncograptus is descended from Isograptus caduceus which, on arriving at a certain stage of development, has the proximal parts of the stipes in coalescence and that
1947, 27(0):101-107,109,110,416.
Abstract:The subject of this study is a small collection of specimens made by Misch during his field work in the rugged and little-known region of northwestern Yunnan (P. Misch, 1945) and brought to the United States for study when on leave from the National University of Peking. Field data has been contributed by
1947, 27(0):111-122,417.
Abstract:In the province of Fukien there are five distinct rock series of Permian age iucluding the Uralian limestone. Their lithological characters are sometimes markedly different from those of contemporaneous rocks of neighbouring provinces. This can be accounted for by the different conditions of deposition, the elucidation
1947, 27(0):123-140,418,420.
Abstract:The city of Kweilin is surrounded by the hills which are entirely composed of limestones of the Devonian age. The limestones may be classified into two groups. The lower one is the thinly bedded, dark gray, more or less crystalline dolomitic limestone attaining a thickness of about 80 meters with the base not (?)x-
1947, 27(0):141-161,421.
Abstract:The promulgation by Professor Grabau of his Pulsation Theory has stimulated the interest of Paleozoic stratigraphers throughout the world in the intercontinental correlation of their formation and faunas. The degree to which Professor Grabau's theory will be accepted by stratigraphers generally wi
1947, 27(0):163-170.
Abstract:Through the kindness of Mr. H. Y. Hsia, Director of the Geological Survey of Kiangsi Province, I have received a small collection of vertebrate remains collected by Mr. J. C. Chang, member of the same institute. It was derived from a cave deposit in Lopinghsien about 130 km. N.E.E. of Nanchang, the capital city of Kiangsi. During the 22nd annual meeting of the Geological Society of China, held at Nanking, late October, 1946 Mr. Hsia, in name of Mr. Chang, has made
1947, 27(0):171-192,422,423.
Abstract:Since the appearance of my former short article on the Silurian rugose corals from Yunnan(16), new material have accumulated, among which the more important are the collections of Professor H. C. Chang~1 and of Messrs. H. Y. Ma and S. S. Ssutu~2 in 1944 from northern Yunnan. Additional collections
1947, 27(0):193-204,424,425.
Abstract:With many years residence in Kunming and from several geological trips to different parts in Yunnan, we have obtained some information of the Triassic stratigraphy and its distribution. As a whole the Triassic formations are well developed and widely distributed in this province. They consist of both continental and marine
1947, 27(0):205-228.
Abstract:The study of the sedimentary rocks, stimulated in part by the rise in importance in petroelum geology, is no longer a neglected field. The interest in sedimentology has indeed become wide-spread and the field is at present being attacked by the petrologic-mineralogic approach which employs criteria that can become usable best when put on a quantitative basis. The old stratigraphic-palaeontologic approach, for which criteria used with success in a quantitative way, is culminated by the work of Haug (1) and Grabau (2). Hang first recognized the important distinction between clastics and non-clastic sediments. Grabau followed the suit to divide the sedimentary rocks into three groups: atmogenic hydrogenic and biogenic. These again are subdivided according to composition and texture but the textural subsivisions are treated more important than the compositional ones. The introduction of textural terms such as rudvtes, arenytes and lutytes for the exogenic rocks and spherites, granulite and pulverite for the endogenic rocks has
1947, 27(0):229-242.
Abstract:Although the geological work in China has been carried for a period of more than thirty years, little is done from the mineralogical and petrological viewpoint. Especially regarding igneous petrology, detailed study seems rather scarce. In the summer of 1920 during his geological reconnaissance of
1947, 27(0):243-252,426,430.
Abstract:For forty years the stratigraphical and biological position of the species Camarocrinus asiaticus (1) (2) from the Nyaungbaw beds of Burma and the equivalent beds of western Yunnan has been a moot question. The general opinion appears to be that it is of the nature of a float or the specialized ro
1947, 27(0):253-263.
Abstract:This paper summarizes the conclusions drawn from the accumulated data supplied by many visitors to Szechuan. Hundreds of reports cover different branches of observation from which valuable facts afford to solve the problem here concerned. The successive crustal movements, the formational distribut
1947, 27(0):265-272.
Abstract:In research of the structure of crystals, an X-ray rotation goniometer would always be placed at hand. Among those the Schiebold rotation goniometer for cylindrical film~1 has been proved to be more satisfactory in the observation of the crystal symmetery than others. The principle of this goniome
1947, 27(0):273-297.
Abstract:The Silurian sections to be described in the present paper were taken in 1944 along the Szechuan-Kueichow highway from Chumipu, about 12 kilometers north of the Tungtzu city in northern Kueichou, to Kuanyinchiao in the Chichiang dis-
1947, 27(0):299-319.
Abstract:Baron F. RICHTHOFEN, the famous geographer and geologist, in his monumental five-volume "China" discusses in length the formation of the North China plain. Dealing mainly with the plain of Peiping-Tientsin he distinguishes two major divisions: one higher, that he calls "declivity" (Abdachung) lyin
1947, 27(0):321-346,431,435.
Abstract:In summarizing the geological events, it is revealed that the main structur in Kwangsi, the Epsilon structure, was not accomplished to its present status in one orogeny, but in successive periods. The early stages, although rudimentary, served a postive controlling factor on sedimentation. Eight s
1947, 27(0):347-358,436,438.
Abstract:For the various copper deposits studied during the year 1940 in the three southwestern provinces of Szechuan, Sikang and Yunnan, the possibilities of their supergene enrichment, a vital problem for the value of these deposits, are sum marized in the following paper from field evidences alone. Micr
1947, 27(0):359-365.
Abstract:In April, 1943, the writer had an opportunity to visit the districts of Kianghua and Lanshan in southwestern Hunan. The observed area is structurally an elongated dome, trending NW-SE. It is composed essentially of metamorphosed slates in its central part and of sandstones and limestone forming th
1947, 27(0):367-372,439.
Abstract:In the Western Hills of Peiping, there is a series of sandstone intercalated with shales and conglomerate which generally lies between the Permo-Carboniferous Yangchiatun Coal Series below and the Jurassic Mentoukou Coal Series above. It was first found by Prof. L. F. Yih in 1920 and named as the
1947, 27(0):373-387,440.
Abstract:In the summer of 1945, through the reconnaisance work of several iron and coal fields in the Weining Shueicheng area, the writer had the opportunity of observing the geology along the route. As a result, he found a wealth of facts and recognized many features concerning tectonics, which are rather interesting from the geomechanical point of view. Among the most important features is the arcuate form of an anticlinal end in the vicinity of Weining city. Both Kno (1) and Wang (2) have considered it as the expression of an arc or the reflex are of the Pakang System established by Lee (3). In view of its origin, however, the
1947, 27(0):389-398,441,443.
Abstract:The petrofabric analysis by means of X-ray was first suggested by Professor B. Sander, and a Debye-Scherrer photograph of a slate was taken to show the inhomogenity of the rock fabrics. However the method of analysis and interpretation was not extensively developed. Rocks of cryptocrystalline text
1947, 27(0):399-408.
Abstract:~~
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