收稿日期: 1995-06-12
修回日期: 1995-10-17
网络出版日期: 1996-07-01
ORGANIC MATTER IN ORE DEPOSITS: CHARACTERI STICS CLASSIFICATION AND ANALYTICAL METHODS
Received date: 1995-06-12
Revised date: 1995-10-17
Online published: 1996-07-01
庄汉平，卢家烂 . 金属矿床中的有机物质:特征、分类方案与研究方法[J]. 地球科学进展, 1996 , 11(4) : 372 -377 . DOI: 10.11867/j.issn.1001-8166.1996.04.0372
Organic matter in ore deposits (OMOD) acts as an important indicator of ore genesis.This paper deals with(1) the characteristics of OMOD with respect to time and lithology of reserivors and type,abundance,source,maturity of OMOD;(2)grade 3 classification based on the end members of kerogen,bitumen and solid carbon;and (3) reviews on prevalent analytical methods such as molecular organic geochemistry,organic petrology,physical chemical method,stable isotope,thermodynamic equilibrium calculation,and model experiments on organic metal interactions.
[1]庄汉平,卢家烂.与有机质有成因联系的金属矿床.地质地球化学，1996,(待刊).
[2]涂光炽.中国层控矿床地球化学(第二卷).北京:科学出版社，1988.27- 36.
[3]傅家漠，刘德汉，卢家烂，等.层控矿床有机地球化学研究的几个问题.中国科学院地球化学研究所有机地球化学开放实验室年报(1988).北京:科学出版社，1988. 174- 185.
[4]Cize A P, M arming D A C. Aspects of the organic geochemistry and petrology of metalliferous ores. In: Engel M H, Macko S A，ed. Organic geochemistry. New York: Plenum Press, 1993. 565-580.
[5]Sverjensliy D A.Oil field brines as ore}orming solutions. Econ Ceol, 1984, 79: 23-37.
[6]陈庆年，贾蓉芬，刘德汉.丹寨汞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实验室年报(1986).贵阳:贵州人民出版社，1986. 145- 158.
[7]Peabody C E, Einaudi M T .Origin of petroleum and mercury in the Culver-Baer Cinnabar Deposit. M ayacmas District, California. Econ Ceol, 1992, 87: 1078-1103.
[8]庄汉平，冉崇英，何明勤，等.楚雄盆地铜、盐、有机质相互作用与砂岩铜矿生成.地质学报，1996,(待刊).
[9]Stach E,Mackowsky M-H, Teichmuller M，et al. Coal Petrology. Cebriider Borntraeger, Berlin, 1982. 535.
[10] Mossman D J, Thompson-Rizer C L. Toward a working nomenclature and classification of organic matter in Preciambrian( and Phanerozoic) sedimentary rocks. Precimbrian Research, 1993, 61:171-179.
[11]Durand B. Kerogen-Insoluble Organic M atter from Sedimentary Rocks .Paris: Technip, 1980. 224- 334.
[12]刘德汉.碳酸盐中沥青在研究油气生成演化和金属矿床中的应用.有机地球化学文集.北京:科学出版社，1986. 133-138.
[13]Tissot B P,Welte D H. Petroleum formation and occurrence(second revised and enlarged edition).New York:Springer-Verlag, 1984. 699.
[14]施继锡，李本超，傅家谟，等.有机包裹体及其与油气的关系.中国科学(B辑)，1987, ( 3) : 318- 326.
[15]Etminan H, Hoffmann C F. Biomarkers in fluid inclusions: A new toolin constraining source regimes and its implicanons for the genesis of Mississippi Valley-type deposits. Geology, 1989, 17: 19- 22.
[16]Kesler S E, Jones H D, Furman F C, et al. Role of crude oil in the genesis of M ississippi valley-type deposits: Evidence from the Cincinnati arch. Geology, 1994, 22: 609-612.
[17]Tompkins L A, Rayner M J, Groves D I. Evaporites: In situ sulfur source for rhythmically anded ore in the Cadjebut Mississippi Valley-type Pb-Zn eposit, Western Australia. Econ Ceol, 1994, 89: 467-492.
[18]Anderson C M .Precipition of Mississippi Valley-type ores. Econ Ceol, 1975,70:937- 942.
[19]Cirodano T H. A preliminary evaluation of organic ligands and metal-organic complexing in Mississippi Valley type ore solutions. Econ Ceol, 1985, 80: 96- 106.
[20]Saxby J D. The significance of organic matter in ore genesis. In:Wolf K H ed. Handbook of Stratabound and Stratriform ore Ore Deposits. New York: Elsevier, 1976. 111-133.
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