Assessment of generation temperatures of crude oils

被引:32
作者
Sajgó, C [1 ]
机构
[1] Hungarian Acad Sci, Lab Geochem Res, H-1112 Budapest, Hungary
基金
美国国家科学基金会;
关键词
generation of crude oil; generation temperature; maturity parameters; molecular ratios; homolog ratios;
D O I
10.1016/S0146-6380(00)00097-8
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Biological marker maturity parameters were used to estimate the minimum HC generation temperatures of crude oils from Eastern Hungary. More than 50 oils and oil shows were analysed. Molecular- and homologous-ratios of biological marker compounds (triterpanes, steranes, mono- and triaromatic steroid hydrocarbons) were used as maturation parameters. The oils have at least five maturity stages, i.e. they have been generated under different thermal conditions. The highest reservoir temperature in each group was chosen as the best estimate of the groups' temperature just below the generation temperature, i.e. reservoirs of the group might be expected to be at shallower depths (lower temperatures) than those of the generation zone due to vertical migration into pools. For each maturation level, a threshold temperature range for genesis was inferred from reservoir temperatures; they are from 130-135 degreesC for the least mature oils to 210-215 degreesC for the most mature oils. In the least mature oils cracking was not observed, hence carbon-carbon cracking reactions had not taken place during their genesis. The most mature oils an intensively cracked oils; they are almost condensates. Two major genetic groups (families) of oils were found in the area. Both are present in each maturation level. The effects of migration were checked, and no influence on maturation was found. A number of the oils are in overpressured reservoirs within, or just above, the zone of the present-day active oil generation, hence the present-day temperatures of the pools must have been maximum temperatures. Contrary to the traditionally accepted temperature range for petroleum generation-maturation reactions (50-150 degreesC), there is strong evidence from this study that the onset of oil generation requires temperatures higher than 130 degreesC and is still proceeding above 215 degreesC. (C) 2000 Published by Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:1301 / 1323
页数:23
相关论文
共 131 条
[51]  
Lopatin N.V., 1971, AKADEMIYA NAUK SSS G, V3, P95
[52]   C26-C29 TRIAROMATIC STEROID DERIVATIVES IN SEDIMENTS AND PETROLEUMS [J].
LUDWIG, B ;
HUSSLER, G ;
WEHRUNG, P ;
ALBRECHT, P .
TETRAHEDRON LETTERS, 1981, 22 (34) :3313-3316
[53]  
Mackenzie A. S., 1983, Advances in Organic Geochemistry, P496
[54]  
Mackenzie A.S., 1984, Advances in Petroleum Geochemistry, P115, DOI DOI 10.1016/B978-0-12-032001-1.50008-0
[55]   MOLECULAR-PARAMETERS OF MATURATION IN THE TOARCIAN SHALES, PARIS BASIN, FRANCE .3. CHANGES IN AROMATIC STEROID HYDROCARBONS [J].
MACKENZIE, AS ;
HOFFMANN, CF ;
MAXWELL, JR .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1981, 45 (08) :1345-1355
[56]   MOLECULAR MEASUREMENTS OF MATURITY FOR LIAS-DELTA SHALES IN NW GERMANY [J].
MACKENZIE, AS ;
LEYTHAEUSER, D ;
ALTEBAUMER, FJ ;
DISKO, U ;
RULLKOTTER, J .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1988, 52 (05) :1145-1154
[57]   MOLECULAR-PARAMETERS OF MATURATION IN THE TOARCIAN SHALES, PARIS BASIN, FRANCE .4. LABORATORY THERMAL ALTERATION STUDIES [J].
MACKENZIE, AS ;
LEWIS, CA ;
MAXWELL, JR .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1981, 45 (12) :2369-2376
[58]  
MACKENZIE AS, 1980, THESIS U BRISTOL
[59]   THE STABILITY OF HYDROCARBONS UNDER THE TIME TEMPERATURE CONDITIONS OF PETROLEUM GENESIS [J].
MANGO, FD .
NATURE, 1991, 352 (6331) :146-148
[60]   THE ORIGIN OF LIGHT CYCLOALKANES IN PETROLEUM [J].
MANGO, FD .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1990, 54 (01) :23-27