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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2008-01
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Scientific research frontiers and considerable questions of carbonate diagenesis

HUANG Si-jing,WANG Chun-mei,HUANG Pei-pei,ZOU Ming-liang,WANG Qing-dong,GAO Xiao-yongState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China  
Carbonate diagenesis is an important branch in carbonate sedimentology,especially in carbonate reservoir sedimentology.Recently,there have been remarkable advances on carbonate diagenesis in the following aspects: 1) the geometry and petrogenesis of dolomite hydrocarbon reservoir,particularly referring to the review and reappraisal on dolomitization models cited by many sedimentologists for a long time;2) the mechanism of structurally controlled hydrothermal alteration of carbonate reservoirs,concerning the origin of hydrothermal dolomite and its effects on hydrocarbon reservoir,especially the influences of hydrothermal fluids on carbonate diagenesis in deep-burial setting;3) renewals of classic diagenesis theories of carbonate and challenges to past diagenesis theories that people have been using until now,some new sights of diagenesis in marine-meteoric mixing-zone and marine-burial environments should make us to reappraisal the understanding of carbonate diagenesis;4) wide application of strontium isotope composition to marine carbonate sedimentology,including isochronous correlation of sedimentary sequences,directly dating marine sediments,and interaction of water-rock during diagenesis.However,some following questions existing in the carbonate diagenesis need us to pay more attentions to: 1) the most important dissolving fluids to carbonates are probably H2S and CO2 as byproducts of sulfate reduction in deep-buried setting with sulfate minerals,but carbonates are more soluble in relatively low temperature,which is socalled retrograde solubility;2) a temperature difference(ΔT) for cooling water to dissolve carbonates can be implemented by following two geological processes: ① fluids flowing upward along faults,showing the importance of faults in carbonate diagenesis;② tectonic uplift,suggesting the significance of burial history related to tectonics in carbonate diagenesis;3) the first thing controlling Sr content in dolomite is the crystalline chemistry habits,lower distribution coefficient of Sr into dolomite results in pervasively lower Sr content in dolomite,thus,people can not only depend upon contents of Sr in dolomite to evaluate the characteristics of dolomitization fluids,and a lower content of Sr in dolomite can not indicate that dolomitization fluid is irrespective to seawater;4) remove of SO4~(2-) related to sulphate reduction may place a premium on the dolomitiztion or precipitation of dolomite,and the presence of SO4~(2-) in fluid may increase the rate of dolomite dissolution.
【Fund】: 国家自然科学基金资助项目(4067207240472068)
【CateGory Index】: P588.245
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9 Ma Xiuzhen Yin Mingshan (Lanzhou Institute of Chemical Physics, Academia Sinica, Lanzhou) Wang Dazhen ( Institute of Microbiology, Academia Sinica, Beijing );SULFATE-REDUCING BACTERIA AND THEIR GEOBIOCHEMICAL ROLE OF SALT LAKE SEDIMENTS OF CHINA[J];Acta Sedimentologica Sinica;1987-02
10 CAI Chun fang 1,3 GU Jia yu 2 CAI Hong mei 3 1(Institute of Geology and Geophysics, CAS, Beijing 100029) 2(Petroleum Exploration and Development Institute, CNPC, Beijing 100083) 3(Jianghan Petroleum Institute, Jingzhou, Hubei 434102);Effect of Hydrocarbon Emplacement on Diagenesis of Silurian Sandstone of Central Tarim Basin[J];Acta Sedimentologica Sinica;2001-01
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