松辽盆地嫩江组介形类毛孔显微构造特征研究

STUDY ON THE PORE MICROSTRUCTURE CHARACTERISTICS OF OSTRACODA FOSSIL IN NENJIANG FORMATION OF SONGLIAO BASIN

本文对松辽盆地白垩纪嫩江组介形类化石壳体表面毛细管孔的显微构造特征研究表明，白垩纪嫩江组沉积时期，松辽古湖盆应为一陆相沉积体系，其水体性质应为淡水—少盐水的古湖泊环境。

The study on microstructure characteristics of the five pores on the surface of ostracoda at Nenjiang Formation of Songliao Basin in Cretaceous shows that during the depositional period of Nenjiang Formation in Cretaceous,Songliao Basin should be a continental depositional system and palaeolacustrine enviroment and furthermore its water body property should be fresh saltish.