东海盆地新生代沉积环境
- 中国海洋石油总公司、海洋石油勘探开发研究中心
作者简介:
王国纯,男,48岁,高级工程师,石油地质.
- 收稿日期:
1990-04-30
- 刊出日期:
1992-06-10
摘要: 东海盆地是新生界为主的沉积盆地,根据地震和钻井资料分析,可划分为四套沉积层序:白垩统—古新统、始新统、渐新统—中新统和上新统—第四系.沉积环境经历了浅海、海陆交替相→海湾相→河湖交潜相→平原河流相→浅海(开阔海)相的发育历程.
Cenozoic Sedimentary Environment in East China Sea Basin
- China Offshore Oil Exploration and Development Research Center
- Received Date:
1990-04-30
- Publish Date:
1992-06-10
Abstract: East China Sea Basin is a large Cenozoic sedimentary basin developed in the eastern continental shelf area of China, with 250000km of the area and over 12000 m of maximum thickness. Four depositional se quences have been interpreted in the basin, based on the study and analysis of seismic stratigraphy, drilling lilhological and paleontologic data and so on. These sequences are sequence Ⅰ late Cretaceous-Paleocene with the largest thickness of 85000m, distributed only in the west of the basin, sequence Ⅱ Eocene with maximum thickness of 6000 m in the east and about 1000m in the west, sequence ⅢOligocene-Miocene with up to 5000m of largest thickness, and sequence Ⅳ Pliocene-Quaternary with sedimentary thickness of approximately 2000m. The boundaries between these sequences are all angle unconformity. These sequences are characterijed by different evolution, lithology, paleontology and depositional environment. Sedimentary environments were analysed: Neritic fades and alternative marine and terrestrial facies appeared in the west of the basin with sea transgression from southeast in late Cretaceous-Paleocene. In Eosene neritic facies developed predominantly in the southwest of the basin, and in the east of Oligocene fluviolacustrine facies appeared and developed only in the basin alternative estuary and lake fades occured. the east, and in Miocene fluviolacustrine facies developed dominantly with swamp subfacis. in the both south and north extremities some local areas were affected by sea water. From Pliocene to Quaternary sedimentary environment changed gradually from fluvial to littoral and neritic facies. The article indicates various assemblages of source rocks, reserviors and sealing rocks formed by different sedimentary enviton ments. Main source rocks are Paleoeene in the west of the basin and Eocene in the east of it, and late Cretaceous is possible significant source rock and Oligocene and lower Miocene is favorable source rocks in the east.. Even though only a few wells have been drilled in the basin potential prospects have been show already. It is believed with our confidence that there are geological conditions to form large oil and gas field m East China Sea Basin
王国纯, 朱伟林. 东海盆地新生代沉积环境[J]. 沉积学报, 1992, 10(2): 100-108.
| 引用本文: |
王国纯, 朱伟林. 东海盆地新生代沉积环境[J]. 沉积学报, 1992, 10(2): 100-108.
|
Wang Guochun, Zhu Weilin. Cenozoic Sedimentary Environment in East China Sea Basin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 100-108.
| Citation: |
Wang Guochun, Zhu Weilin. Cenozoic Sedimentary Environment in East China Sea Basin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 100-108.
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