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超压地层中镜质组反射率的计算
引用本文:肖丽华,孟元林,张连雪,韦阿娟,李军,张文才,殷秀兰,王志国. 超压地层中镜质组反射率的计算[J]. 石油勘探与开发, 2005, 32(1): 14-17
作者姓名:肖丽华  孟元林  张连雪  韦阿娟  李军  张文才  殷秀兰  王志国
作者单位:1. 大庆石油学院
2. 大庆石油学院;中国地质大学,北京
3. 中国石油大港油田勘探开发研究中心
4. 中国地质大学,北京;中国石油大港油田勘探开发研究中心
5. 中国地质环境监测院
基金项目:国家"十五"重大科技攻关项目(2001BA605A08)国家自然科学基金项目(4037102)
摘    要:已有的研究表明,超压可以抑制镜质组的热演化、增加反应活化能。在EASY%R0模型的基础上,通过超压调节化学动力学反应活化能,建立了超压条件下镜质组热演化的化学动力学模型Pa%R0,并根据黄骅坳陷歧北洼陷受超压抑制和未受超压抑制的R0实测资料,确定了有关模拟参数。歧北洼陷港深48井明显超压(压力系数1.2~1.6),用Pa%R0模型所预测的有机质成熟度和生烃时间与用EASY%R0模型预测的明显不同,超压对R0的抑制可达0.1%~0.3%,可使烃源岩进入生油门限的时间推迟1~4.4Ma。图2参34

关 键 词:超压 镜质组反射率 成岩作用 烃源岩 盆地模拟 黄骅坳陷 歧北洼陷
文章编号:1000-0747(2005)01-0014-04

Vitrinite reflectance modeling in the over-pressured formations
XIAO Li-hua,MENG Yuan-lin,ZHANG Lian-xue,WEI A-juan,LI Jun,ZHANG Wen-cai,YIN Xiu-lan,WANG Zhi-guo. Vitrinite reflectance modeling in the over-pressured formations[J]. Petroleum Exploration and Development, 2005, 32(1): 14-17
Authors:XIAO Li-hua  MENG Yuan-lin  ZHANG Lian-xue  WEI A-juan  LI Jun  ZHANG Wen-cai  YIN Xiu-lan  WANG Zhi-guo
Affiliation:Daqing Petroleum Institute, Hebei 066004, China;Daqing Petroleum Institute, Hebei 066004, China;Oil and Gas E&D Technology Research Center, Dagang Oilfield Company, PetroChina, Tianjin 300280, China;Oil and Gas E&D Technology Research Center, Dagang Oilfield Company, PetroChina, Tianjin 300280, China;Oil and Gas E&D Technology Research Center, Dagang Oilfield Company, PetroChina, Tianjin 300280, China;China University of Geosciences, Beijing 100083, China;China Institute of Geo-enviorenmental Monitoring,Beijing 100081,China;Daqing Petroleum Institute, Hebei 066004, China
Abstract:The studies indicated that overpressure could retard vitrinite reflectance and increase activity energy. Using the vitrinite reflectance from both the overpressure well and the normally pressured well, a new vitrinite reflectance kinetic model Pa% Ro incorporating overpressure retardation is developed, in which overpressure modifies activity energy. The model was tested in Qibei Sub-sag of Huanghua Depression. The results suggest that the maturity and timing of the onset of hydrocarbon generation is different significantly from those predicted by EASY%.Ro. The vitrinite reflectance values are retarded by 0. 1%-0. 3% in the overpressure formations with the pressure coefficient of 1. 2-1. 6, and the time of source rocks entry into oil generating threshold is delayed by 1-4. 4Ma.
Keywords:overpressure  vitrinite reflectance  diagenesis  source rock  basin modeling  Huanghua Depression  Qibei Sub sag
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