1) Tongjiang area of central Sichuan
2) chuanjiang region in upper and middle reaches of Yangtze River
3) Zhongchuan area
Characteristics of fluid inclusions in the gold deposits within Zhongchuan area, western Qinling and their geological significance;
Zhongchuan area is located in the southern margin of the Li-Min forland basin which is caused by yangtze plate's subducting to Huabei plate,and it situated in the region between Lixian-taoping deep fault and its subfault Lixian-luoba fault.
4) central Sichuan Basin
Thick-bed sand body genesis and oil-gas migration pathway in the forth member of Xujiahe Formation of Upper Triassic in the central Sichuan Basin;
Genetic types and main controlling factors of sandbodies in second and fourth members of Xujiahe Formation,upper Triassic,Central Sichuan Basin;
Typical gas reservoirs and main controlling factors of reservoir-forming of Upper Triassic Xujiahe Formation in central Sichuan Basin
5) middle of Sichuan basin
The paper mainly discussed the conditions of hydrocarbon accumulation in An Pingdian-Gao Shiti structure,middle of Sichuan basin.
The accumulation mechanism of natural gas is still an unsolved problem in the Lower Triassic Jialingjiang Formation of Moxi-Longnüsi area in the middle of Sichuan Basin.
6) Zhongjiang Area
Serious collapsing is always existed in the drilling process in Shaximiao formation of Zhongjiang area, which brings technical difficulty in drilling operation and huge economic loss.