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2009 Vol. 27, No. 6

Mineralogical and Geochemical Identification for Diagenetic Settings of Paleocaves and FracturesFilling & Vugs Calcites in Carbonate:Taking Wells S79 and S85 for example 
QIAN Yixiong
2009, 27(6): 1027-1032.
Abstract:
Based on observation of core of the Middle and Lower Ordovician carbonate in Wells S85 and S79, a wide rangegeochemical methods has been used to characterize the diagenetic settings of paleocaves and fractures filling & vugs calcites and to deciphe...
Geochemical Characteristics of Dolomites in Lower Triassic Feixianguan Formation, Northeast Sichuan, China 
WANG Yi
2009, 27(6): 1043-1049.
Abstract:
The lower Triassic Feixianguan Formation is a shallow marine carbonate sequence with shale and evaporates. The edge of carbonate platform commonly developed some oolitic banks, which are dolomitized. The oolitic bank dolomites are the most important ...
Sedimentary Characteristics of Shallowwater Deltas in Chang8 Subsection of Yanchang Formation, Jiyuan area
HAN Yonglin
2009, 27(6): 1057-1067.
Abstract:
Jiyuan area is in the middle of the western Ordos Basin and its sedimentary facies is controlled by provenance from northeast, northwest and south directions in Late Triassic epoch. Detailed studies have been made on the rock types, sedimentary struc...
Depositional Model of Gravity Flow of Slope in Large Down Warped Lake Basins
WANG Ying
2009, 27(6): 1076-1083.
Abstract:
Slope break belt is the most favorable setting for gravity flow development. Slope break belt can be developed in Lake basins and has the similar characteristics with one in continental slopes. Therefore, the study on depositional model and distribut...
Forced Regression and Normal Regression Deposition of Basin with Continental Shelf Slopebreak: A case study on Zhujiang and Hanjiang Formations of Pearl River Mouth Basin
XIE Lihua
2009, 27(6): 1093-1100.
Abstract:
The question about the deposition and the corresponding systems tract in forced regression is always the domestic and foreign focal point of argument. Integrated with sequence stratigraphic depositional model which was established by Exxon Corporatio...
Division of HighResolution Sequence Stratigraphy of Jiufotang Formation Outcrop in Kazuo Basin
WEI Hengfei
2009, 27(6): 1109-1115.
Abstract:
On the basis of 106 kilometers measured sections and detailed research of sedimentary characteristics and evolution of Jiufotang Formation in Kazuo Basin,according to facies sequence relationship and the genetic significance of Calcium Carbonate and ...
Characteristics of Sequencebased Lithofacies and Paleogeography of the Changxing Formation in the Eastern KaijiangLiangping Intraplatform Trough
DONG Xia
2009, 27(6): 1124-1130.
Abstract:
Based on the study of sedimentary facies and sequence stratigraphy, Changxing Formation is a thirdorder of type Ⅱ sequence and subdivided into three systems tracts: SMST, TST, and HST. The lithofacies paleogeographic map based on systems tract as th...
Distribution Characteristics and Geological Significances of Tuff Interlayers in Yanchang Formation of Ordos Basin
QIU Xinwei
2009, 27(6): 1138-1146.
Abstract:
Tuff interlayers distributing widely in Yanchang Formation in Ordos Basin, lots of cores which containing tuff interlayer were observed, then summarized the log curves characteristics of tuff, which represent by relatively low SP, high GR, R and AC, ...
Rare Earth Element Records of the Lower Paleogene Sediments in the Sanshui Basin and Their Paleoclimate Implications
CHEN Liang
2009, 27(6): 1155-1162.
Abstract:
The concentration of rare earth elements (REE) was determined in the Lower Paleogene core sedimentary rock from the Sanshui Basin. The ∑REE contents range from 7.06 to 230.01 μg/g, with an average value of 142.32 μg/g, close to that of Upper Continen...
Analysis of Effect of Water and Sediment Load and Evolution Trend of theDifferent Channel Patterns in the Lower Yellow River
WANG Suiji
2009, 27(6): 1163-1171.
Abstract:
It is an important science problem that braiding, meandering and straight channel patterns appeared in the lower Yellow River. Some researches have studied this problem in different aspects. However, some existent insufficiencies still need to study...
Hg Occurrence and Distribution in Sediments of the Nanhai Lake 
SA Ruli
2009, 27(6): 1178-1183.
Abstract:
The sequential extraction procedure was chosen for the study of speciation of Mercury in sediments of the Nanhai Lake. The fractions of watersoluble and exchangeable Hg are easy to release to the overlying water, and the sum of them account for 30.8...
Distribution Characteristics of Glycerol Dialkyl Glycerol Tetraether Lipids in Lake Dianchi Sediments
XIONG Yongqiang
2009, 27(6): 1191-1198.
Abstract:
Glycerol dialkyl glycerol tetraether lipids in the Lake Dianchi sediments were determinated based on bulk and molecular organic geochemical analyses of a lake sediment core (63 cm in length). The results indicate that the Lake Dianchi sediments have ...
Molecular Organic Geochemistry of Langshan Formation in Selincuo Sag, Coqen Basin, Central Tibet, China
WANG Licheng
2009, 27(6): 1199-1207.
Abstract:
Coqen Basin is the second largest marine basin in Tibet Plateau. Carbonate rocks of the Lower Cretaceous Langshan Formation is one of the most important hydrocarbon source rocks. Although having good conditions for petroleum preservation, Selincuo Sa...
沉积与能源、矿产
Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone
ZHANG Tianfu
2009, 27(6): 1033-1042.
Abstract:
Oolitic limestone is an crucial oil reservoir. Through dissolution kinetics experiment under normal temperature and pressure, this paper discussed dissolution kinetics characteristics and morphology evolution of oolitic limestone. The result indicate...
Geochemical Characteristics of Doushantuo Cap Carbonate (Dolostone) and Discovery of Beltanelliodes Podolicus Fossil in
YANG Ruidong
2009, 27(6): 1050-1056.
Abstract:
The basal Doushantuo Formation in Qingzhen County, Guizhou Province, China, consists of mudstones, muddolostones, dolosandstones, thin dolostones and thick dolostones. The preservedwell and abundant carbon discform fossils, 2~15 mm in diameter, ...
Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin
ZOU Caineng
2009, 27(6): 1068-1075.
Abstract:
The study of deep water sedimentation has developed fifty years. The misuse of term “turbidite” to deposits of deep water is common. Then the denial of Bouma sequence as the tubidite facies sequence and related fan depositional mode, the study on dee...
Genetic Combination of the Sandbody in the Fourth Members of Xujiahe Formation(Upper Triassic) and Its Influence on Oil and Gas Reservoirs
XIE Wuren
2009, 27(6): 1084-1092.
Abstract:
The sandbody of Upper Triassic Xu 4 member in central Sichuan basin is thick,continuous sedimentation,and characterized by shoreshallow lacustrinedelta frontdelta plain which is proximal.During sedimentation, there were different accommodation spa...
Sequence Stratigraphy Characteristics and Main Controlling Factors of the Tectonic Active Basin:As an example from Permian of the Kebai Area in the northwestern Junggar Basin
ER Chuang
2009, 27(6): 1101-1108.
Abstract:
The Kebai fault zone in the northwestern Junggar Basin is a largescale imbricate thrust system which originated in Permian. The tectonic activity played an important role in controlling the sedimentary process. Permian is a mixing accumulated format...
The Sequence Stratigraphics Characteristics of Upper Permian in the Northeastern Sichuan Basin
LI Fengjie
2009, 27(6): 1116-1123.
Abstract:
On the basis of stratigraphic theory and the analysis of sedimentary facies, lithology and lithofacies and the changing of accommodation of field profile, sequence stratigraphy are researched to the upper Permian at Yanggudong profile in Dukou town, ...
Identification of Common Facies Indicators of Seismites in Simulated Experiments
YAN Jihua
2009, 27(6): 1131-1137.
Abstract:
Sedimentary facies indicators are the best effective criteria to identify seismites. In the flume experiments to simulate seismoturbidites, several typical facies indicators of seismites are found in soft sediments, such as synsedimentary faulting, ...
Paleosalinity Records to Sea Level Change of the Northern Margin of the South China Sea in Early Jurassic
XU Zhongjie
2009, 27(6): 1147-1154.
Abstract:
A largescale transgression occured in early Jurassic in the eastern Guangdong Province, the continental margin of South China Sea. The sea level change is recorded by the variation of paleosalinity. The ratios of Sr/Ba and B/Ga reflecting the paleos...
现代沉积与环境
Modern Sedimentation Rates in Prydz Bay, Antarctic
YU Peisong
2009, 27(6): 1172-1177.
Abstract:
Using the 210Pb dating methods in the sediment cores, the modern sedimentation rates in Prydz Bay (Antarctic) are estimated. The results show that the modern sedimentation rates are mainly controlled by marine primary productivity in upper water a...
Discovery and Geological Significance of Red Clay in the Liulin Section in the West Part of Lüliang Mountains
LI Jianxing
2009, 27(6): 1184-1190.
Abstract:
A special aqueous gravel bed, which underlies the red clay and is mainly composed of red clay lumps and calcium nodules, was found at Weijiawa village of Liulin county in the west part of Lüliang Mountains. Sedimentological study shows that the clast...
油气地质地球化学
Geochemical Characteristics and Reservoir Formation of Cambrian Heavy Oil of Well Tadong 2 in Tarim Basin
TANG Youjun
2009, 27(6): 1208-1215.
Abstract:
Studying the geochemical characteristics and formation history of heavy oil from Well Tadong 2 is of great importance to clarify the oil accumulation of Tarim marine crude oil. The writer synthetically apply the isotope mass spectrogram, chromatogram...