摘要
莺歌海盆地第三系有巨厚的欠压实泥页岩,泥丘的发育受北西向的红河大断裂及其派生的南北向雁行断裂所控制。泥丘本身就是生烃岩,它所孕育的异常高温高压之巨大潜能,是有机质成熟生烃和烃类排出运移的动力;而它伴生的不同类型的构造所组成的泥丘隆起构造带则是油气运移聚集的有利场所。
The formation and evolution of mud-mounts in the Yinggehai Basin are closelyrelated to hydrocarbon generation,migration and accumulation.1.The mud mounts are distributed in Oligocene Yacheng Formation and the MioceneSanya and Meishan Formations.The formation,evolution and distribution is decided bymaterial base—the rapidly deposited,high thickness and undercompacting mud shales,regional dynamics and gravity factor.2.Mud mounts themselves are source rocks;abnormal high temperature and highpressure produced by their evolution is the motive force for hydrocarbon generation andmigration,especially for high pressure natural gases soluted in water.3.The mud mount uplift structural belts are mostly distributed in the central part ofthe basin or the deeper parts of the depressions that are favourable locations for hydrocar-bon migration and accumulation.It is predicted that the pools of mud mounts within thebasin are mainly anticline,semianticline and noze types,and then faulted-noze type.4.The mud mount uplift structral belts in the central part and the fault-block struc-tural belts in the southeast,having abundant hydrocarbon source and fine accumulationand preservation conditions,are favourable enrichment zones,and should be taken as im-portant targets for recent exploration;No.1 fault-structural belt could be taken as explo-ration target in the future due to its poor accumulation and preservation conditions.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
1990年第4期436-445,共10页
Oil & Gas Geology
