HOU Qijun; MENG Qian and ZHANG Ge
, 2004, 31(4): 874-0.
Abstract (
)
Download PDF (
)
Knowledge map
Save
Abundant fluid conclusions, existed in the authigenic minerals, are developed in the sandstone of the Fuyang reservoir, Qijia-Gulong area, Songliao Basin. The homogeneous temperature of saltwater inclusion, which is co-developed with organic conclusion, is conspicuous for three peaks revealing the three stages of hydrocarbon injection of Fuyang reservoir. During the first hydrocarbon injection stage, the homogeneous temperature of inclusion is 90-120℃, with the organic inclusions distributing in the late quartz secondary increase edge, concrescence fracture of quartz grains and calcite cement. And, the organic inclusion in the concrescence fracture of quartz grains is injected in the homogeneous temperature of 100-110℃, and may be account for a tectonic movement under the homogeneous temperature between 90-100℃ and 110-120℃ which results in the fracturing of quartz grains. Evidence of the hydrocarbon injection is further represented by the oil trace or bitumen, representing possibly the main stage of hydrocarbon injection, existed between the secondary concrescence edge and calcite cement. The second hydrocarbon injection happened in the process of infilling of calcite vein and concrescence of quartz fracture with the homogeneous temperature of 120-150℃, and the bitumen in the calcite vein demonstrate the relatively large amount of hydrocarbon injection in this stage, and therefore prohibiting the growth of authentic minerals. The third stage of hydrocarbon injection is recorded and represented by the secondary concrescence of quartz edge, and revealing the homogeneous temperature of 160-170℃. The laser Laman spectrum indicates that the evolution degree of organic matter in the early oil and gas injection period is lower compared with that in the late injection period.