中國油氣區(qū)第三系

出版時間:1997-05-01  出版社:葉得泉、Zhong Xiaochun、Yao Yimin、 Yang Fan 石油工業(yè)出版社 (1997-05出版)  作者:葉得泉 等 著  

內(nèi)容概要

  《中國油氣區(qū)第三系(英文版)》主要內(nèi)容包括:CHARACTERISTICS OF THE DISIRIBUFION OF TFRTIARY IN CHINA AH.AND GAS-BEARING BEGIONS、TERTLARY BIOTAS OF CHINA AH.AND GAS-BEARING REGIONS、APPLICATION OF SEISMIC STRATIGRAPHY,MAGNETOSTRSTIGRAPHY ISOTOPLC CHRONOSTRATIGRAPHY ANG EVENT STRATIGRAPHY METHODS TO STRATIGAPHIC CORRLATIONS、CORRELATIONS OF TERTIARY STRATA IN CHINA AH.AND GAS-BEARING REGIONS TERTLARY PALAEOENVIRONMENT OF CHINA OH.AND GSA-BEARING REGIONS等。

書籍目錄

CHAPTER 1 CHARACTERISTICS OF THE DISTRIBUTION OF TERTIARY IN CHINA OIL AND GAS-BEARING REGIONS 1.1 Widespread Depositional Basins 1.2 Dominance of Nonmatine Deposits, with a Variety of Deposition Types 1.3 Tertiary Development under Control of Tectonic Movement 1.4 Extremely Abundant Fossils 1.5 Frequent Volcanic Activities in East China with an Extensive Distribution of Volcanic Rocks 1.6 Rich Mineral Resources CHAPTER 2 TERTIARY BIOTAS OF CHINA OIL AND GAS-BEARING REGIONS 2.10stracodes 2.2 Foraminifers 2.3 Gastropods 2.4 Bivalves 2.5 Vertebrates 2.6 Sporopollen 2.7 Dinoflagellates and Acritarchs 2.8 Charophytes 2.9 Calcareous Nannofossils 2.10 Fossil Plants CHAPTER 3 APPLICATION OF SEISMIC STRATIGRAPHY,MAGNETOSTRATIGRAPHY,ISOTOPIC CHRONOSTRATIGRAPHY ANG EVENT,STRATIGRAPHY METHODS TO STRATIGRAPHIC CORRELATIONS 3.1 Application of Seismic Stratigraphy to Stratigraphic Correlations 3.2 Isotopic Geological Age Determination of Volcanic Rocks 3.3 Age-Determination of Palaeogeomagnetism 3.4 Application of Stable Isotope Stratigraphy and Event Stratigraphy CHAPTER 4 CORRELATIONS OF TERTIARY STRATA IN CHINA OIL AND GAS-BEARING REGIONS 4.1 Typical Tertiary Sequences 4.2 Basis for Tertiary Stratigraphical Correlations 4.3 Correlations of Tertiary Strata 4.4 Correlations with Tertiary Normal Sequence of Europe and America 4.5 Discussion on Tertiary Boundaries CHAPTER 5 TERTIARY PALAEOENVIRONMENT OF CHINA OIL AND GAS'-BEARING REGIONS 5.1 Tertiary Palaeovegetation and Palaeoclimate 5.2 Tertiary Palaeobiogeographical Provinces and their Controlling Factors in China 5.3 Discussions on the Paleogene "Transgression" in East China Oil and Gas-bearing Regions CHAPTER 6 DIVISION OF TERTIARY OIL-GENERATING PERIODS AND PREDICTION OF OIL AND GAS PROSPECTS IN OIL AND GAS-BEARING REGIONS OF CHINA 6.1 TertiaryOil Source Rocks Disttibution in Chinese Oil and Gas-beating Regions 6.2 Influential Factors on Development of Dark-Coloured Strata and Hydrocarbon Potential 6.3 Division of Tertiary Oil-Generating Periods 6.4 Application of Stratigraphical Palaeontological Studies to Prediction of Oil and Gas Potential 6.5 Prediction of Tertiary Oil and Gas Prospects CONCLUDING REMARKS REFERENCES

章節(jié)摘錄

版權(quán)頁:   插圖:   1.1.7 Northern South China Sea Shelf Oil and Gas-bearing Region This region mainly includes the Zhujiangkou (Pearl River Mouth),Beibuwan,Yinggehai and Southeastern Qiongya Basins in the Northern sea area of the South China Sea together with some other local areas of Hainan and Guangdong Provinces.In this region the Paleogene mainly belongs to continental deposits; the transgression began from Late Oligocene and became further expanded up to the Neogene.As a result,in this region the Neogene is mainly developed with marine deposits,which are extensively distributed,with a thickness of more than 3,500m.This region also represents a distributive area of variegated elastic rocks. The coast-line of Mainland China is as long as 18,000km,with an extremely vast expanse of territorial and neighbouring sea areas.Within the sea areas of Bohai,Huanghai,East China Sea and South China Sea,there are 16 depositional basins with developed Tertiary,mostly belonging to those of inheritance type and newborn type,with a total area attaining 1,955,500km2.It is doubtless,therefore,that there exist extremely broad prospects in the Tertiary oil and gas exploration over the sea areas of China. However,in the Xizang Region,the Tertiary is not very well-developed,and therefore exploration for oil and gas has not been carried out to a great extent therein.Accordingly,the Xizang Region is not included in the research Project on the Tertiary of China Oil and Gas-bearing Regions.In the Xizang Region,there are 18 Mesozoic and Cenozoic depositional basins,includong 9 Tertiary basins of the newborn type,which are generally studied in a lower degree. 1.2 Dominance of Nonmarine Deposits,with a Variety of Deposition Types In China,the nonmarine Tertiary,with a great thickness,is extensively distributed all over the depositional basins of various genetic types throughout the conutry.As compared with marine deposits,the continental deposits obviously occupy a dominant position,while marine deposits are distributed within a relatively narrow scope.

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