摘要
通过景谷盆地晚第三纪三个介形类组合特征分析,说明生物所具有的继承性,又因环境的变化出现不同的种属类型,壳面的装饰和保存状况也发生了变化。景谷盆地晚第三纪中新世中期生物繁盛,有机质丰富,为油气生成提供了物质基础,同时有利的水介质条件和快速的沉积,为有机质的保存和转化成烃类提供了外界条件。
Based on Ostracoda fossils collected from Neogene in Jinggu Basin, Yunnan Province, three Ostracod assemblage zones are established, as follows:1. Potamcoypris-Candoniella Assemblage zone; (Early Miocene)2. Herpetocypris-Metacyplis Assemblage Zone; (Middle-late Miocene)3. Leucocythere-llyocypris Assemblage Zone; (Pliocene)According to the abundance of Ostracoda with preservad state of their shell, the authorgives a discussion about the relation between the organic matter abundance and depositionalspeed as well as the Ostracoda and Gas and Oil generated in Jinggu Basin。
出处
《石油学报》
EI
CAS
CSCD
北大核心
1992年第2期198-201,共4页
Acta Petrolei Sinica