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作 者:卓勤功
机构地区:[1]石油大学
出 处:《石油实验地质》2005年第2期169-172,共4页Petroleum Geology & Experiment
基 金:中国石油化工股份有限公司科研项目(P00018)
摘 要:流体异常高压控制着烃源岩的成烃机理和油气运聚成藏。超压促进沙四上亚段富硫烃源岩的生烃,而对贫硫的沙三中下亚段烃源岩生烃起抑制作用。因而沙四上亚段烃源岩早生、早排、成熟度较低,生成的油气充注凹陷外围及上部圈闭;沙三中下亚段烃源岩晚生、晚排、成熟度较高,生成的油气充注凹陷内部及下部圈闭。流体异常高压还能形成油气运聚的通道。所以,隐蔽输导体系的预测是今后岩性油气藏勘探的关键。The abnormal high-pressure of fluid controls the hydrocarbon-forming mechanism of source rocks and the migration and accumulation of oil and gas. Overpressure promoted the hydrocarbon generation of sulphur-rich source rocks in the upper sub-member of Es^4; by contraries, it restrained the hydrocarbon generation of sulphur-poor source rocks in the middle and lower sub-members of Es^3. Thus, in the former situation, hydrocarbon generated and discharged early, its maturity was lower, and it filled the peripheral and top traps of sags; in the latter, hydrocarbon generated and discharged late, its maturity was higher, and it filled the inner and lower traps of sags. The abnormal hygh-pressure of fluid also formed passages for hydrocarbon migration and accumulation. For the future, the forecast of subtle transportation systems is the key of exploration for lithological reservoirs.
关 键 词:异常高压 成烃机理 运聚成藏 隐蔽输导体系 济阳坳陷
分 类 号:TE122.1[石油与天然气工程—油气勘探]
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