论文详情
大型挤压构造事件对油气成藏的影响
石油实验地质
2009年 31卷 第1期
阅读:149
查看详情
Title
INFLUENCE OF LARGE-SCALE TECTONIC COMPRESSION EVENTS ON THE HYDROCARBON ACCUMULATION
作者
苗洪波
陈红汉
王立武
江涛
邱玉超
崔炳辉
刘清伟
Authors
Miao Hongbo
Chen Honghan
Wang Liwu
Jiang Tao
Qiu Yuchao
Cui Binghui
Liu Qingwei
单位
中国地质大学, 资源学院石油系, 武汉, 430074
2. 吉林油田公司, 勘探开发研究院, 吉林, 松原, 138001
3. 中国石油大学, 资源与信息学院, 北京, 102249
Organization
China University of Geosciences, Wuhan, Hubei 430074, China
2. Exploration and Production Research Institute of Jilin Oilfield Company, Songyuan, Jilin 138000, China
3. China University of Petroleum, Beijing 102249, China
摘要
传统石油成因理论认为有机质成熟度主要受温度、时间与压力等因素的控制。依据松辽盆地勘探实践经验认为热演化程度受温度控制明显,只要温度高,烃源岩可在短时间内大量生烃。构造运动不仅可以产生大量的热,使烃源岩生烃、排烃过程具有突发性,而且挤压作用可以促进烃源岩的排烃作用、运移作用。另外,构造运动又可以形成一系列的圈闭,从而使油气从生成到聚集的过程可以在短时间内完成。因此,在挤压构造发育的区域,即使烃源岩埋藏较浅,也具有一定的排烃能力,形成工业性油气聚集。基于这一认识,应该改变烃源岩埋藏浅就不能排烃的这一常规理念,把盆地边部构造变形较强的区域也纳入勘探视野。
Abstract
According to traditional hydrocarbon genesis theory,it is accepted that organic maturity is affected by temperature,time and pressure.After summarizing exploration practices,it reveals that thermal maturity of organic matter is mainly controlled by temperature.So long as the temperature is high enough,substantial hydrocarbon can be generated from source rock.Tectonic movements do not only produce great amount of heat,but also make hydrocarbon generation and expulsion abruptly.Compressive process promote the hydrocarbon generation and migration.In addition,tectonic movements can form a set of traps,which shorten the time from generation to accumulation.Therefore,in areas where tectonic compression are well developed,though shallow buried source rock,they also have the capacity for hydrocarbon expulsion,and can form economic oil reservoirs.Based on these findings,the traditional theory that shallow source rock can not expulse oil should be broke,and regions of marginal basin with intense structural deformation should be taken into the exploratory frontier.
关键词:
烃源岩;
生烃;
排烃;
油气运移;
构造运动;
松辽盆地;
伊通盆地;
辽河盆地;
Keywords:
source rock;
hydrocarbon generation;
hydrocarbon expulsion;
hydrocarbon migration;
tectonic movement;
the Songliao Basin;
the Yitong Basin;
the Liaohe Basin;
DOI
https://doi.org/10.11781/sysydz200901063