高尚堡扇三角洲湖体背景的微体古生物分析

费安玮

doi:10.11743/ogg19970111

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高尚堡扇三角洲湖体背景的微体古生物分析
ANALYSIS OF MICROPALEONTOLOGY IN LACUSTRINE FAN DELTA OF GAOSHANGPU
1997年18卷第1期页码：59-64
网络首发：1997-03-25，

纸质出版：1997
DOI： 10.11743/ogg19970111
稿件说明：

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费安玮. 高尚堡扇三角洲湖体背景的微体古生物分析[J]. 石油与天然气地质, 1997,18(1):59-64. DOI： 10.11743/ogg19970111.

Fei Anwei. ANALYSIS OF MICROPALEONTOLOGY IN LACUSTRINE FAN DELTA OF GAOSHANGPU[J]. 1997, 18(1): 59-64. DOI： 10.11743/ogg19970111.

摘要

采用介形类与孢粉、藻类研究相结合

定性与定量分析相结合的微体古生态学方法

分析高尚堡油田沙河街组三段扇三角洲沉积体在湖盆中所处位置及古环境。该扇三角洲主要发育在滨、浅湖环境

介形类主要成分为Candona

Huabeinia及Candoniela并以浅水型的Candona占优势;孢粉含量通常高于藻类;藻类相继以疑源类Granodiscus

Leiosphaeridia或甲藻类Parabohaidina

Conicoidium为主体

总体上代表了淡微咸水的滨、浅湖环境。

Abstract

According to the study made on the paleoecology of Ostracoda

sporo pollen and algal fossils collected from the fan delta of the third member of the Shahejie Formation in Gaoshangpu Oilfields

it is considered that the fan delta developed in littoral shallow lake environment The main elements of Ostracoda are Candona

Huabeinia and Candoniella with shallow water Candona as the the predominant one The content of the sporo pollen is usually higher than that of algae;the main elements of the algae are Granodiscus

Leiosphaeridia or Parabohaidina and Conicoidium All of the fossils reflect fresh to brackish water in littoral to shallow lake environment