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Genesis of the Maku Hematite Deposit, Weining, Kueichou

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地质学报 1942年第Z1期 169-175页

作者： C. J. PENG (geological survey of china)

INTRODUCTION It was not until C: C. Wang’s work’ was carried out in 193. that the Maku iron deposit of the Weining district, western Kueichou (Fig. 3., has become known among mining engineers and economic geologists... 详细信息

关键词： Kueichou Weining

Petalocrinus form the Shihniulan Limestone of Wuchuan

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地质学报 1949年第Z1期 93-96页

作者： A. T. MU (geological survey of china)

The materials described in the present paper were collected by Mr. F. H. Chia from the Shihniulan limestone at Kingchikou near Sankengssu, about 25 km NE of the Wuchuan city, NE Kueichou. Three species of Petalocrinus are identified, namely, Petalocrinus inferior Bather, P. inflatus sp. nov., and P. chiai sp. nov. All of them are only represented by arm-fans. The genus is not uncommon in the Silurian strata of china, but it is not yet described heretofore.

关键词： view Petalocrinus form the Shihniulan Limestone of Wuchuan

Permian Stratigraphy and Palogeography of Fukien

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地质学报 1947年 111-122+417页

作者： C. S. KAO (geological survey of china)

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 neigh... 详细信息

关键词： ogeography of Fukien Permian Stratigraphy and Pal

Pleistocene Morainic and Non-Morainic Deposits in the Taqlaq Area,North of Aqsu,Sinkiang

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地质学报 1944年第Z1期 139-169页

作者： T. K. HUANG (geological survey of china)

With 5 Plates. INTRODUCTION In April 1943. while exploring the foothills of the southern Tienshan near the prosperous oasis of Aqsu-Wensu, I have repeatedly come across a series of well-preserved morainic deposits alo... 详细信息

关键词： Pleistocene Morainic and Non-Morainic Deposits in the Taqlaq Area,North of Aqsu,Sinkiang

Notes on the Bauxite Deposits of Kueichou,with Special Reference to Their Variation in Quality

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地质学报 1944年第Z1期 98-114页

作者： C. J. PENG (geological survey of china)

The discovery of bauxite from a number of places in Kueichou in 1941 made by Dr. S. S. Yoh and his colleagues [13. is of economic as well as scientific significance. In the following year, the writer, in collaboration with Dr. C. Y. Li, had an opportunity of making an investigation of the three deposits found, namely, Yunwushan;, Wangbi;and Wangkuan;. Though a

关键词： Notes on the Bauxite Deposits of Kueichou,with Special Reference to Their Variation in Quality

On a New Form of Fusulinid

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地质学报 1948年第Z2期 249-251页

作者： T.S.KUO (geological survey of china)

Of the taxonomic characteristics of Fusulinidae it is the septa of thefusulinid that are highly *** septal folding is quite uniformand regular and the intensity of the septal folding from the top to the bottommargins of the septa and from poles to the median portion of the test isequally strong and *** in axial section,the septa appear as a

关键词： On a New Form of Fusulinid Form

Tertiary Calcareous Nannofossil Biostratigraphy in the North Part of the South china Sea

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Acta Geologica Sinica(English Edition) 1991年第3期65卷 321-338,343-344页

作者： Duan Weiwu and Huang Yongyang Gangzhou Marine geological survey, Ministry of Geology and Mineral Resources, Guangzhou Chang Zhijun and Sun Sheping Guangzhou Marine geological survey Ministry of Geology and Mineral Resources Guangzhou

The marine Tertiary sequence in the north part of the South china Sea may be divided into 18 LateOligocene to Pliocene calcareous nannofossil zones and one unnamed Eocene assemblage based on an analysisof calcareous nannofossils from 40 offshore boreholes. The unnamed Eocene assemblage has been found onlyon the northeast margin of the Zhujiangkou basin. The 18 cakareous nannofossil zones of the Late Oligoceneto Pliocene were deposited in succession, but their development degrees are different. Among the 18 calcareousnannofossil zones, those corresponding to Martini's (1971) NN4- NN5 zones, NN11 zone and NN13.NN15zones are well developed, relatively persistent laterally and also widely distributed. They are the importantmarkers for the stratigraphical subdivision and correlation of the Upper Tertiary between the various basins inthe north part of the South china Sea. Based on the calcareous nannofossils and the sedimentsry features coup-led with the foraminifer zonation in certain basins, the present paper discusses the sedimentary characteristicsof the marine Tertiary and as well as the distribution and development of the sedimentary hiatus in the *** calcareous nannofossil markers for the Upper / Lower Tertiary and the Quaternary / Tertiary boundaries,and the characteristics and geological significance of the reworked calcareous nannofossils are also discussed inthe paper.

关键词： Tertiary Calcareous Nannofossil Biostratigraphy in the North Part of the South china Sea

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URANIUM ORE－FORMING　FOSSIL　HYDROTHERMAL　SYSTEMS　IN　XIANGSHAN，jiangxi　province，EAST　china

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Scientia Geologica Sinica 1996年第4期 515-522页

作者： Sun Zhanxue(East china geological Institute, Linchuan, jiangxi 3.4000)

ＵＲＡＮＩＵＭＯＲＥ－ＦＯＲＭＩＮＧＦＯＳＳＩＬＨＹＤＲＯＴＨＥＲＭＡＬＳＹＳＴＥＭＳＩＮＸＩＡＮＧＳＨＡＮ，ＪＩＡＮＧＸＩＰＲＯＶＩＮＣＥ，ＥＡＳＴＣＨＩＮＡＳｕｎＺｈａｎｘｕｅ（ＥａｓｔＣｈｉｎａＧｅｏｌｏｇｉｃ... 详细信息

ＵＲＡＮＩＵＭＯＲＥ－ＦＯＲＭＩＮＧＦＯＳＳＩＬＨＹＤＲＯＴＨＥＲＭＡＬＳＹＳＴＥＭＳＩＮＸＩＡＮＧＳＨＡＮ，ＪＩＡＮＧＸＩＰＲＯＶＩＮＣＥ，ＥＡＳＴＣＨＩＮＡＳｕｎＺｈａｎｘｕｅ（ＥａｓｔＣｈｉｎａＧｅｏｌｏｇｉｃａｌＩｎｓｔｉｔｕｔｅ，Ｌｉｎｃｈ...

关键词： ORE FORMING URANIUM FOSSIL HYDROTHERMAL EAST china

Sequence Stratigraphy and Tectonic Environment of the Chartai Group,Inner Mongolia

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Acta Geologica Sinica(English Edition) 1991年第3期65卷 217-235,341-342页

作者： Qiao Xiufu Yao Peiyi Wang Chengshu Tan Lin Zhu Shenyu Zhou Shengde Zhang Yuqing Institute of Geology,Chinese Academy of geological Sciences, Beijing Regional geological survey Party,geological Bureau of Inner Mongolia,Hohhot Sun Sheping Institute of Geology Chinese Academy of Geological Sciences Beijing China

The Middle Proterozoic Chartai Group separated by two unconformities consists of three depositional se-quences: the Shujigou Formation-Zenglongchang Formation (DS Ⅰ), the Agulugou Formation (DS Ⅱ), andthe Liuhongwan Formation (DS Ⅲ). The carbonate platform and back-platform basin are the basic environ-ment model of the Chartai Group. The syndepositional faults on the oceanward side of the carbonate platformand large-scale slumping in the soft sediments are important marks of facies tracts. The newly establishedZenglongchan uplifting, an epeirogenetic uplifting, plays an important role in the formation of thepalaeogeographic framework of the Chartai Group. The stratigraphic correlation between the Chartai Groupand the Bayan Obo Group is made for the first time by using sequence stratigraphic principle and model estab-lished by P.R. Vail. The Chartai Group, which was deposited on the northern passive continental margin of theNorth china platfom, represents the platform cover.

关键词： Sequence Stratigraphy and Tectonic Environment of the Chartai Group Inner Mongolia

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