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1993 Vol. 11, No. 2

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Sedimentation and Environmental Development of Late Proterozoic Luoyu Group, Western Henan
Men Qingren, Hu Jianmin
1993, 11(2): 1-10.
Abstract:
Widely exposed in the western Henan,the Late Proterozoic Luoyu Group consists of sili-ciclastic rocks in the lower section and stromatolite dolostones and dolo-mudstones in the upper section, recording a complete transgressive-regressive depositional...
A Precambrian Andean -Type Flysch: Petrology and Geochemistry of Yangzhanling Flysch in Southern Anhui, China
Xia Bangdong, Ma Xueming
1993, 11(2): 19-26.
Abstract:
A suit of late Proterozoic Sandstones and shales up to 2800m thick is wide-spreaded in Southern Anhui province. It has been identified by many researchers as a flysch according to a series of characteristics,such as rhythms,grading textures,contempor...
Analysis of Microfacies,Microfacies Associations and Sedimentary Environments of Carbonate Rocks of the Middle Devonian in Xicheng Pb-Zn Orefield
Song Chunhui, Wu Anbin
1993, 11(2): 34-42.
Abstract:
The Xicheng Pb-Zn orefield locates in Gansu Province, is one of the most famous ore-fields in China. Its controlling horizon are Anjiacha and Xihanshui formations of the middle Devonian,and its ore-bearing rocks belong to marine clastic and carbonate...
Effects of Sedimentation and Diagenesis on Distribution of Gold of Banna Formation,Middle Triassic in NW Guangxi,Sw China
Liu Jinzhong, Fan Delian
1993, 11(2): 51-57.
Abstract:
Banna Formation is the source bedds and host rocks of fine-impregnation gold ore deposits in Northwest Guangxi. The formation is turbidites with 150-5000m thick,and composed of sandstone,siltstone,mudstone and mirl. Through statistical analysis of go...
Silicification in Wongfu Phosphorus Deposits in Guizhou,China
Chen Doufu, Chen xianpei
1993, 11(2): 58-54.
Abstract:
Wongfu phosphorus deposits is a kind of sedimentary phosphorus deposits formed in Doushantou formation with era of Sinian,widely associated with silicified rocks which were formed by means of replacing original rock(such as phosphorate,dolomite.etc. ...
Storm Deposits in Member III of Feixianguan Formation,Triasic Series in Zhongliang Mountain,Chongqing
Hu Zhishui, Zhao Yongsheng
1993, 11(2): 84-90.
Abstract:
Storm current is a special current caused by strom in littoral and sea bottom which has both characters of gravitationsl and tractive current. The limited base effected by storm is called as storm wave base. When sediments deposit on the base,it woul...
Composition and Distribution of Suspended Load in Sea Water off Zhujiang River Mouth and Its Vicinal Shelf
Lu Mengyu, Chen Shuzhen
1993, 11(2): 99-104.
Abstract:
The suspended load in sea waters off Zhujiang (pearl) River Mouth and on its vicinal shelf was studied by grain-size analysis and mineralogical and microbiological assays on more then 100 specimens collected in four cruises in 1985 and 1986. The dist...
Three New Structural Terpenes and Their Geochemical Significance in Recent Sediment of Qinghat Lake
Wang Zhaoyun, Fan Pu
1993, 11(2): 113-117.
Abstract:
Three new structural tricyclic diterpenes are first reported in this paper. They are examined in the recent sediments of Qinghai Lake and their eluting time is between bicylic ter-panes of long chain and tetracyclic diterpanes of m/z 123 mass chromat...
Studies of Kerogen From Baise Basin,Guangxi-Also on Relationship of Evolution of Kerogen and Clay Minerals
Lu Qi, Liu Huifang, Luo Lijuan, Lei Xinrong
1993, 11(2): 124-132.
Abstract:
Kerogen is the direct original material of oil-forming. To determine the type and the mature degree of kerogen is one of the important work in petroleum geology. While studing the clay minerals of Baise Basin,Guangxi,the authors made some detialed wo...
Contents
Types and Reservoiring Performance of Dolostones of the Lower Paleozoic in Eastern North-China Platform
Jin Zhenkui, Feng Zengzhao
1993, 11(2): 11-18.
Abstract:
Dolostones are very common in the Lower Paleozoic of eastern North-China Platform, and can be divided into mud-silt-sized crystalline dolostones and fine-coarse crystalline dolostones. The former includes gypsiferous and non-gypsiferous; the later in...
Trace Fossils From Middle-ordovician Jinsushan Formation, Fuping, Shaanxi and Their Depositional Environments
Li Rihui
1993, 11(2): 27-33.
Abstract:
Characteristized by hemipelagic thinly-bedded lime mudstones interbedded with limestone breccias derived from gravity flow,the Middle-Ordovician Jinsushan Formation yields abundant trace fossils,but the are not evently vertical distributed. A brief d...
The Origin of Dolostone and Its Reservoir Characteristics of Sinian and Palaeozoic,Northwestern Margin of Tarim Basin
Shi Ji'an
1993, 11(2): 43-50.
Abstract:
Massive dodlostone are widely developed in the strata of Sinian, Cambrian, Ordovician and Carboniferous in the northwestern margin of Trim Basin,three types can be divided according to the shape and size of dolomite in them. 1. Dolostone composed of ...
Tempestites and the Environmental Paleoecological Significance of Early Silurian, Nvv Sichuan Area
Zhang Tingshan, Hou Fanghao, Gao Weidong, Lan Guangzhi
1993, 11(2): 55-74.
Abstract:
Several Early Silurian storm-wave genesis of bioclastic limestone beds which deposited on the muddy shelf have been recognized from NW Sichuan area. The Early Silurian deposited at the NW margin of the S-China Paleo-plate tectonically and it has the ...
Sequence Structural Characteristics of the Devonian Volcanoclastic Turbidites in Northern Xinjiang and Their Geological Significance
Gong Yiming
1993, 11(2): 75-83.
Abstract:
The volcaniclastic turbidites which are characterized by more than 25% pyroclastic contents and by the Bouma sequence are widely distributed in the Upper Devonian of east Jung-gar, the lower part of the Lower Devonian and the Upper Devonian of west J...
Storm-Deposits in Upper Proterozoic in Southeastern Huabei Sino-Forean Massif
Wang Xiang, Wang Zhan
1993, 11(2): 91-98.
Abstract:
The area of northern Jiangsu and Anhui provinces locates on the southeastern edge of Huabei massif (Sino-Korean massif),and is one of the key areas for the division and correlation of Upper Proterozic in China. Since late 80's,some geologists have re...
Sedimentary Features of Liaohe Estuary and the Evolution of Dynamics of the Tidal Banks
Bao Yong'en, Huang Shuiguang
1993, 11(2): 105-112.
Abstract:
Sea area around Liaohe Estuary refer the region between Liaohe Estuary to the east and Xiaolinghe Estuary to the west,which's water depth is defined as 10m shallower. Drainages where enter into the sea are liaohe.Shuangtaihe, Dalinghe and Xiaolinghe ...
Distributive Characteristics of Bio-markers in Modern Sediments of Dachaidan Lake, Qaidam Basin
Tuo Jincai, Shao Hongshui, Huang Xingzhen
1993, 11(2): 118-123.
Abstract:
Modern mud of Dachaidan Lake and the mudstone of the Pliocene sampled from Well Nan-4 both were formed under drought climate. GC and GC-MS had been used to the saturated fraction of hydrocarbons of the samples and the results revealed that;the distri...
Study on the Origin of the Dolostone Intercalcated in the Black Shales in Middle Permian Lucaogou Formation Eastern Part of Southern Margin of Junggar Basin
Zhang Xiaobao
1993, 11(2): 133-140.
Abstract:
The black shales and dolostones intercalcated with them had been researched petrologi-cally and geochemically of middle Permian Lucaogou Formation,eastern part of southern. Margin of Junggar Basin. The great similarity between them has been found. Ba...