Fluid interaction mechanism and diagenetic reformation of basement reservoirs in Beier Sag, Hailar Basin, China |
LI Juan,WEI Pingsheng,SHI Lanting,CHEN Guangpo,PENG Wei,SUN Songling,ZHANG Bin,XIE Mingxian,HONG Liang |
Fig. 9. Simulation of burial history and thermal evolution of Beier Sag. Q—Quaternary; E—Paleogene; K2q—Upper Cretaceous Qingyuangang Formation; K1y2+3—Lower Cretaceous Yimin Formation members 2+3; K1y1—Lower Cretaceous Yimin Formation member 1; K1d2—Lower Cretaceous Damoguaihe Formation member 2; K1d1—Lower Cretaceous Damoguaihe Formation member 1; K1n2—Lower Cretaceous Nantun Formation member 2; K1n1—Lower Cretaceous Nantun Formation member 1; K1t—Lower Cretaceous Tongbomiao Formation; Pb—Permian Budate Group; C—Carboniferous. |