准噶尔盆地红山嘴地区克拉玛依下亚组孔隙结构特征及影响因素

doi:10.3969/j.issn.1673-8926.2008.04.012

Lithologic Reservoirs ›› 2008, Vol. 20 ›› Issue (4): 65-70.doi: 10.3969/j.issn.1673-8926.2008.04.012

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Pore structure and influencing factors of Lower Karamay Formation in Hongshanzui area of Junggar Basin

ZHOU Fengjuan¹，WANG Zhenqi¹，ZHI Dongming²，GUAN Lijun³，HU Qingqin⁴，WU Xuewei⁵

1. College of Geosciences， Yangtze University， Jingzhou 434023， China； 2. Research Institute of Exploration and Development， Xinjiang Oilfield Company， PetroChina， Urumqi 830013， China； 3. Exploration Department of Shenzhen Sub-Company， CNOOC， Shenzhen 518067， China； 4. Research Institute of Geophysical Prospecting， Zhongyuan Oilfield Branch, Sinopec， Puyang 457000， China； 5. Development Department， Jidong Oilfield Company， PetroChina， Tanghai 063200， China

Online:2008-12-15 Published:2008-12-15

Abstract

Abstract:

The cast thin section, scanning electronic microscope, cast image analysis and mercury injection analysis are applied to analyze the pore structure of the Lower Karamay Formation reservoir in Hongshanzui area. The main pore type of the Lower Karamay Formation reservoir is secondary dissolved pore. The throat type is lamellar or curved lamellar, mainly of moderate and fine throat. The Lower Karamay Formation is mainly composed of type Ⅲ-Ⅳ reservoirs. The main influencing factors of the pore structure are sedimentation and diagenesis, and the cementation and dissolution are dominant factors.

Key words: reef and shoal, logging facies, seismic facies, reservoir prediction, Upper Permian Changxing Formation, eastern Sichuan-northern Chongqing area

ZHOU Fengjuan，WANG Zhenqi，ZHI Dongming，GUAN Lijun，HU Qingqin，WU Xuewei. Pore structure and influencing factors of Lower Karamay Formation in Hongshanzui area of Junggar Basin[J].Lithologic Reservoirs, 2008, 20(4): 65-70.

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