Several Problems of Organic Geochemistry in the Forming of Some Sediment-reformed Deplsits
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摘要: 本文通过大量模拟实验结果说明有机质在层控矿床矿源层的形成以及后期改造——活化迁移阶段可能起到重要作用。同时,根据原油相对水溶液相中的金属元素的强烈萃取能力,认为在石油形成和初次运移阶段,金属元素可能在原油相——非水体系中发生运移和富集。Abstract: Both laboratory and field studies show that organic matter could play an important role in the forming of sediment-reformed deposits. 1.Forming sediment source rock Humic and fulvic acids have a strong tendency to complex and to absorb metal elements, one gram fulvic acid can complex and absorb 188mg Cu, 165mg Zn, and 276mg Cd respectively; one gram sea algal fregment can combine 58-78μg Au. Humic and fulvic acids are high molecular- weight, weak acid polyelectrolyts, and they are coagulated by strong electrolyte(sea water); biodetritus and clay mineral usually get to setttl in sea water and fresh water. Then humic matter and metal elements carried by it would be able to deposit and to form source rock. 2.The role in mobilization and migration of metal elements The determining results show that interlayer water and oil-field water were rich in organic acids and cyclic compounds containing O, S, P, N, etc.; while their character is simillar with ore-forming solution(called low temperature ore-forming solutions). The experimental studies suggest:(1) The solubility of mineral(sphalerite and galena) is much higher in solutions containing dissolved organic compounds than in inorganic solutions(generally 4-17 times);(2) the four complexes studied, lactic acid-Zn complex, EDTA-Zn and fulvic acid-Zn have high thermal stability, their thermal decomposition temperatures are in the rang of 140-240℃. 3.The migration and accumulation of metal elements in crud oil(waterree system) Experimental results suggest that crude oil has a strong tendency of extracting metal elements from aquous solutions, 54-90% of Au, Cu, Pb, Zn can be extracted solubility of mineral in mineral-crude oil-solution system is much higher than that of single aquous solution. The authors suggest that some mud-rock and shale had ever ben "double source rock", metal elements were mobilized. When petroleum was formed and migrated.
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[1] (1) 尹汉辉,喻茨玫,张国新,卢家烂,1984,层控铅锌矿床的地球化学,涂光炽等著《中国层控矿床地球化学》第1章,科学出版社,I 3-66页。
(2) 卢家烂,1988.溶解有机质与多金属元素相互作用的模拟实验研究,涂光炽等著《中国层控矿床地球化学》科学出版社,282-296页.
(3) 卢家烂,王玉荣,1984,实验地球化学,涂光炽等编《地球化学》第八章,上海科技出版社.
(4) 卢家烂,袁自强,1986,有机-锌络合物稳定性的实验研究,地球化学I期,第66-77页.
(5) 陈庆年,贾蓉芬,刘德汉,1986,丹寨汞一金矿床有机质与金属的某些特征.中国科学院地球化学研究所有机 地球化学开放研究实验室研究年报(1986),贵州人民出版社,145-158页.
(6) 郑明华,刘建明,1986,论浙江治岭头金银矿床的成矿物质来源,矿床地质,5卷1期,39-52页.
(7) 涂光炽等,1988,《中国层控矿床地球化学》,第三卷,科学出版社.
(8) 傅家漠,刘德汉,贾蓉芬,施继锡,1988,碳酸岩有机地球化学-在石油、天然气、煤和层控矿床成因及评介中的应用,科学出版社,172-193页.
(9) Beveridge T.J., Meloche J. D., Fyfe W.S. and Murray R.G.E., 1983. Appl Environ Microbiol V.45, p.1094-1108.
(10) Collies A.G., I975, Geochemistry of oil field waters. Elservier Scientific Pub.Company. I85-219
(11) Cooper B.S. and Harris R.C.1974 Marine pollut. Bull, V.S, p.24-26
(12) Coveney, Jr, R.M., 1988,美国中西部宾夕法尼亚系,富含金属的黑色页岩的分布及成因(摘要),中国科学院地球化学研究所有机地球化学开放研究实验室CC 1988研究年报》科学出版社。
(13) Gatellier J.P. and Disnar J.R.1989, Applied chemistry V.4, p.143-149
(14) Giordano T.H. and Barnes H.L.1981, Econ. Geol, V.76, p.2200--2211.
(15) Hallberg R.O., Bubela B. and Ferguson. J. 1980 Geomicrobiol. 1.V.2, p.99-113.
(16) Hirner A.V., Kritsotakis K. and Tobschall H.J., 1990 Applied Geochomistry V.S, p.491-505.
(17) Idiz E.F,Garlisle D.,. and Kaplan LR. 1986. Applied Geochemistry. V.1,p.573-590
(18) Jackson K.S.. Jonasson LR,and Skippen G.B., 1978. Earth-Science Review, V.14, p.97-146
(19) Nissebaum A. and Swaine D.J., 1976, Geochim. Cosmochim. Acta, V40, p809-816
(20) Piittmann W., Merz C. and Speczik S. 1989. Applied Geochemistry V.4, p.151-161.
(21) Sangameshwar S.R. and Barnes H.L. 1983, Economic Geology V.78, p.1379-1397.
(22) Sver石ensky D.A. 1984. Econ. Geol. V.79, p.23-37.
(23) Williams, 1987, Geochemical and prebiotic systems in comprehensive coordination chemistry(G. wilkinson ect.) V.6, p.843-879.
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