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2000 Vol. 18, No. 1

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Spatial Variations of Channel Patterns
NI Jin ren, WANG Sui ji, WANG Guang qian
2000, 18(1): 1-6.
Abstract:
The formation of channel patterns and its characteristics are important aspects in modern and ancient fluvial system studies, and thus become the main concern for hydraulic engineers, geomorphologists and sedimentologists. So far, there are still som...
Sedimentary Pigment and Its Environmental Signification of East Juyanhai in Inner Mongolia since the Past 2600 Years
QU Wen chuan, WU Rui jin, WANG Su min, ZHANG Zhen ke
2000, 18(1): 13-17.
Abstract:
Organic carbon content in lake sediment is often used to indicate the lake paleoprimary productivity.The main sources of organic carbon include autochthonous lake organism and allochthonous terrestrial plant,and there is complex degradation after dep...
Assessing the Impact of Reclamation Activities on Recent Sedimentation in Victoria Harbour, Hong Kong
PAN Shao ming, SHI Xiao dong, WANG Jian ye, PETER Tanner, LAI ShingLeong
2000, 18(1): 22-28.
Abstract:
The sediments that accumulate in an estuarine environment recorded the information about the history of changes in the source of the material, the rate of deposition and the influence of man. Man's influences on Victoria Harbour are significant. To c...
Model of Grain-size Distribution of the Eolian Deposits in Lanzhou Area and its Paleoclimatic Significances
DAI Xue rong, LI Ji jun, YU Li zhong, SHI Yu xin, WANG Jia cheng
2000, 18(1): 36-42.
Abstract:
The Quaternary eolian deposits in Lanzhou,west of the Loess Plateau,is the thickest area in China as aresult of the geographic position and the topographic conditions.Investigation show that Lanzhou is also a dust-storm frequent area in the present t...
High-Resolution Sequence Stratigraphy of Terrestrial Penglaizhen Formation of Xinchang Gas Field in Western Sichuan
LIU Mei qing, CHEN Yi jun, ZHENG Rong cai
2000, 18(1): 50-56.
Abstract:
According to the data of rock cores, well loggings and seismic interpretations, three order base-level cycles are recognized from Penglaizhen Formation in Xinchang area, which consist of 45-47 short-term base-level cycles, 5 mid-term base-level cycle...
Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data
KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang
2000, 18(1): 63-67.
Abstract:
It is well known that integrated use of outcrop, well-logging and seismic data is the key to sequence stratigraphy. Therefore, how to identify the sequence boundary by well-logging in the lacustrine sediments which are lack in the unconformity is cri...
Late Triassic Deep Water Trace Fossils and Their Sedimentary Environment in the Jinmuda,Rangtang,Sichuan
YANG Feng qing, XIONG Wei
2000, 18(1): 73-79.
Abstract:
The study area,Jinmuda,Rangtang county, Sichuan province is located in the southeast of Aba Mass. During the early period of Late Triassic, deep water detrital sediments, which can be divided into Zhuwo Formation and Xinduqiao Formation, deposited in...
Analysis of Environment-Facies and Process-Facies of the Honggucheng Formation in the Minghe Basin,Gansu Province,China
CAI Xiong fei, LI Chang an, ZHAN Che sheng, GU Yan sheng
2000, 18(1): 89-94.
Abstract:
The Honggucheng Formation lies in the Upper Lower Cretaceous in the Minghe basin, which is like multistory type and cyclic sequences resulting from multiple flood processing deposition. It is characterized by the interchange of structure underwater a...
Depositional Characteristics of Carboniferous and Its Tectonic Significance in Maanqiao Area, Middle Tianshan
YIN Yong, DONG Yu shan, GAO Chang lin, JIANG Jian chun, FAN Xiao lin
2000, 18(1): 100-106.
Abstract:
The Carboniferous strata outcropped in Maanqiao and northern Baluntai area in Middle Tianshan include Maanqiao Formation (late Datang stage) and Sangshuyuan Formation (Weining stage).The strata belong to the mixed sediments of carbonate and clastic r...
Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea A Review. Part II: Duration and Silica Sources
2000, 18(1): 119-126.
Abstract:
The timing and duration of quartz cementation in sandstones have been mainly inferred from diagenetic texture, relationship between pore filling minerals, fluid inclusions and isotopic data. Fluid inclusion temperatures from North Sea reservoir sands...
Geochemical Characteristics and Evaluation on Hydrocarbon Generation Potentials of Source Rocks in Jurassic Eastern Qaidam Basin
YU Hui juan, TUO Jin cai, LIU Luo fu, CHENG Jian fa, ZHAO Lei
2000, 18(1): 133-138.
Abstract:
The geochemical characters of 13 Jurassic source rock samples in the eastern Qaidam basin are studied by means of Rock-Eval, GC-MS, GC-MS-MAT and so on Based on the comprehensive analyses of the organic carbon content, the content and conversion rati...
The Study on Indigenous Characteristics of Organic Matter in Marine Carbonate Hydrocarbon Source Rock with Low Abundance and High Evolution
LI Yan jun, CHEN Yi cai, XU Zhi ming, LU Qiang, SHI Xiao yin, ZUO Zhi feng
2000, 18(1): 146-150.
Abstract:
The indigenous characteristcs of organic matter in carbonate hydrocarbon source rock directly influences the precise evaluation of its hydrocarbon generation capability especially on marine carbonate rock with low organic matter abundance and high th...
Effective Amount of Gas Released from Water and Its Significance
FU Guang, ZHANG Yun feng, CHEN Zhang ming
2000, 18(1): 157-161.
Abstract:
Based on the study of factors influencing the dissolution ability of gas in formation water, this paper analyses the geological conditions for gas to release from water,and points out that the decrease of temperature and pressure, increase of mineral...
Contents
Study of the Slump Structure on the Yellow River Delta During Its in Zero
ZHONG Jian hua, LI Li
2000, 18(1): 7-12.
Abstract:
On the delta during Yellow River in zero,there developed a great number of slump structures,which might be formed near the edge of point bar and channel bar or in the channel developed whithin the point bar or channel bar,as well as in the river cour...
Study on the Magnetic Susceptibility of the Xiashu Loess and the Paleoenvironment Changes in the Middle and Lower Changjiang River
ZHANG Jian jun, YANG Da yuan, CHEN Yue you, LI Xu sheng, JIANG Hong jun
2000, 18(1): 18-21.
Abstract:
The stufy of loess-paleosol sequence reveals the magnetic susceptibility is of indexical significance in identifying loess-paleosol and their progression in the loess section,but also in simulating the changes of paleoenvironment.The magnetic suscept...
A New Geological Theory about Eluvial Zone ——Theory Illuvial on Depth of CaCO3
ZHAO Jing bo
2000, 18(1): 29-35.
Abstract:
In the research of many geological problems about weathered eluvial zone, the conten theory is widely adpoted, which is based on content of chemical composition. Although the content is very important to resolve lots of geological problems, this theo...
Genetic Types of Meter-Scale Cyclic Sequences and Their Fabric Features of Facies-Succession
MEI Ming xiang, XU De bin, ZHOU Hong rui
2000, 18(1): 43-49.
Abstract:
Different types of meter-scale cyclic sequences in stratigraphical records are the outcomes of episodic accumulation of strata related to Milankovitch cycles. They are marked by particular features of facies-successions resulted from different sedime...
Characterestics of Sequence Sedimentary Organic Facies and Distribution of Source Rocks of Majiagou Formation,Lower Ordovician, Ordos Basin
ZHU Chuang ye
2000, 18(1): 57-62.
Abstract:
A sedimentary organic facies is defined as a stratigraphic unit, in which there are the similar characteristics of depositional environment, biological assemblage, diagenetic environment, reduction-oxidation condition, and the genetic type of organic...
Paleoenviromental Significance of Trace Fossils in Tempestite of Qilang Fm.(Middle Ordovician)of Northwestern Tarim Basin in China
FANG Guo qing, LIU De liang
2000, 18(1): 68-72.
Abstract:
The Qilang Formation of Middle Ordovician in northwest Tarim basin is composed of laminae marl and laminae limestone with abundance graptolites and trilobites.This kind of marl and limestone thin alternation is typical L-M (limestone-marl) cycle.Ther...
Petroleum Sporo-Pollen Assemblages of Tarim Basin
JIANG De xin, YANG Hui qiu
2000, 18(1): 80-88.
Abstract:
One hundred sixty-three species of fossil spores and pollen referred to 83 genera extracted from 44 crude oil samples collected from the Tarim Basin were recorded. Based on the investigations of the characteristics of the petroleum sporo-pollen assem...
Fractal Features of Fan-Shaped Depositional Bodies
ZHOU Jiang yu, LIU Chang qing
2000, 18(1): 95-99.
Abstract:
Fan-shaped depositional bodies are those mainly composed of terrigenous coarse deposits and fan-shaped in morphology, including alluvial fan, fan delta, delta and subaqueous fan and so on. They are important exoil-gas targets in oil and gas-bearing b...
Genetic Model of the Deep Water Salt Lake of the Paleogene Sha-4 Member in Dongying Sag
YUAN Jing, ZHAO Cheng Ling, ZHANG Shan Wen
2000, 18(1): 114-118.
Abstract:
There were cyclothems consisted of evaporite rocks,deep color mudstones or shales and deep water turbidity sediments of Peleogene Sha-4 member in Dongying sag,which was salt lake sedimentary assemblage with more than 1000m in thickness.The evaporite ...
Application of Well Logging Information to Analysis on the Effect of Diagenesis in Reservoirs
ZHANG Xiao li, SHEN Ying, CHEN Wen xue
2000, 18(1): 127-132.
Abstract:
Based on the analysis of compression pore evolution, fracture, mineral component and the study of effect of diagenesis stages on reservoirs, the physical base of effects of diagenesis stages on reservoirs is discussed by applying well logging informa...
Controls on Compositional Heterogeneity of Oils in Jiuxi Basin
XIONG Ying, CHENG Ke ming, YANG Zhi ming
2000, 18(1): 139-145.
Abstract:
The physical and chemical nature of petroleum changes with source rock and maturity,although the feature of oil and gas can also be influenced by local biodegadration or water washing.During the process of reservoir filling,some polar compound in cru...
A Quantitative Microscopic Model of Hydrcarbon Accumulation
LUO Ming gao, HUANG Jian quan, TANG Hong
2000, 18(1): 151-156.
Abstract:
Because both migration and accumulation of oil and gas proceeded within the pore space of reservoir,the porosity structures directly have an effect on the accumulation of oil and gas as well as the formation and distribution of oil and gas reservoirs...
Timing on Cave Deposit (Stalagmites) by High-Precision Thermal Ionization Mass Spectrometry (TIMS)
WANG Zhao rong, PENG Zi cheng, SUN Wei dong, JI Shoubin
2000, 18(1): 162-164.
Abstract:
Cave calcium has turned out to be a very important data-bank of paleoclimatic evolution.Stalagmite,flow stone and calcite veins in caves,like tree rings,ice cores,loess and lacustrine deposits,contain precise records of past environmental variation.D...