Reservoir Characteristics and Main Controlling Factors of the Lower Jurassic Tight Sandstone in Eastern Kuqa Depression

ZHANG NiNi; LIU LuoFu; SU TianXi; DAI QiWen; ZHAO YuanYuan

doi:10.14027/j.cnki.cjxb.2015.01.017

Volume 33 Issue 1

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ZHANG NiNi, LIU LuoFu, SU TianXi, DAI QiWen, ZHAO YuanYuan. Reservoir Characteristics and Main Controlling Factors of the Lower Jurassic Tight Sandstone in Eastern Kuqa Depression[J]. Acta Sedimentologica Sinica, 2015, 33(1): 160-169. doi: 10.14027/j.cnki.cjxb.2015.01.017

Citation:

ZHANG NiNi, LIU LuoFu, SU TianXi, DAI QiWen, ZHAO YuanYuan. Reservoir Characteristics and Main Controlling Factors of the Lower Jurassic Tight Sandstone in Eastern Kuqa Depression[J]. Acta Sedimentologica Sinica, 2015, 33(1): 160-169. doi: 10.14027/j.cnki.cjxb.2015.01.017

Reservoir Characteristics and Main Controlling Factors of the Lower Jurassic Tight Sandstone in Eastern Kuqa Depression

doi: 10.14027/j.cnki.cjxb.2015.01.017

ZHANG NiNi^1,2,
LIU LuoFu^{1,2
,},
SU TianXi^1,2,
DAI QiWen^1,2,
ZHAO YuanYuan^1,2

1.
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing 102249;
2.
Basin and Reservoir Research Center, China University of Petroleum (Beijing), Beijing 102249

Received Date: 2013-11-18
Rev Recd Date: 2014-05-12
Publish Date: 2015-02-10

Abstract

The tight sandstone gas of Tarim Basin has a large distribution and great exploration potential, which is an important prospective exploration field of the basin in the future. The Lower Jurassic sandstone in eastern Kuqa depression is commonly tight. It is important for the further exploration and development to strengthen the study of its reservoir characteristics and the main controlling factors. In order to reveal the controlling factors and development mechanism of the Lower Jurassic tight sandstone reservoir in eastern Kuqa depression, by use of the tests of casting section, cathodeluminescence, scanning electron microscope and laser confocal microscopy are applied, together with the geological and logging analyses. The lithology, pore structure characteristics and physical properties are carried out in this paper. The results show that lithic sandstone is the main reservoir rock type, and the rock composition maturity is low while the textural maturity is of medium degree. The pore structure is mainly mesoporous with fine throat and micropore with fine throat. Majority of the porosity values ranges from 4% to 12%, with an average of 8.12%, and the effective air permeability is mainly (0.1~3)×10^-3μm²; On the basis of the comprehensive analyses of sedimentation, diagenesis and tectonics of tight reservoir strata, the studies suggest that the reservoir physical property is mainly controlled by sedimentation, diagenesis and tectonism. The main controlling factors are granularity and compaction.
- reservoir characteristics,
- main controlling factors,
- tight sandstone,
- Lower Jurassic,
- eastern Kuqa depression

References

[1]	Golab A N, Knackstedt M A, Averdunk H,et al. 3D porosity and mineralogy characterization in tight gas sandstones[J]. The Leading Edge, 2010, 29(12): 1476-1483.
[2]	Higgs K E, Zwingmann H, Reyes A G,et al. Diagenesis, porosity evolution, and petroleum emplacement in tight gas reservoirs, Taranaki Basin, New Zealand[J]. Journal of Sedimentary Research, 2007, 77(12): 1003-1025.
[3]	Neves F A, Al-Marzoug A, Kim J J,et al. Fracture characterization of deep tight gas sands using azimuthal velocity and AVO seismic data in Saudi Arabia[J]. The Leading Edge, 2003, 22(5): 469-475.
[4]	Smith T, Sayers C M, Liner C. Introduction to this special section: Tight gas sands[J]. The Leading Edge, 2010, 29(12): 1463.
[5]	Grechka V, Mazumdar P, Shapiro S A. Predicting permeability and gas production of hydraulically fractured tight sands from microseismic data[J]. Geophysics, 2010, 75(1): B1-B10.
[6]	张晓峰,侯明才,陈安清. 鄂尔多斯盆地东北部下石盒子组致密砂岩储层特征及主控因素[J]. 天然气工业,2010,30(11):34-38.[Zhang Xiaofeng, Hou Mingcai, Chen Anqing. Features and main controlling factors of tight sandstone reservoirs in the Lower Shihezi Formation in the northeastern Ordos Basin[J]. Natural Gas Industry, 2010, 30(11): 34-38.]
[7]	张超,李旭平,钟建华,等. 吐哈盆地巴喀油田下侏罗统致密砂岩储层特征及主控因素分析[J]. 山东科技大学学报:自然科学版,2011,30(6):65-72.[Zhang Chao, Li Xuping, Zhong Jianhua,et al. Properties and the main controlling factors of compact sandstone reservoirs in Lower Jurassic series of Baka oilfield in Tuha Basin[J]. Journal of Shandong University of Science and Technology: Natural Science, 2011, 30(6): 65-72.]
[8]	康毅力,罗平亚. 中国致密砂岩气藏勘探开发关键工程技术现状与展望[J]. 石油勘探与开发,2007,34(2):239-245.[Kang Yili, Luo Pingya. Current status and prospect of key techniques for exploration and production of tight sandstone gas reservoirs in China[J]. Petroleum Exploration and Development, 2007, 34(2): 239-245.]
[9]	李建忠,郭彬程,郑民,等. 中国致密砂岩气主要类型、地质特征与资源潜力[J]. 天然气地球科学,2012,23(4):607-615.[Li Jianzhong, Guo Bincheng, Zheng Min, et al. Main type, geological features and resource potential of tight sandstone gas in China[J]. Natural Gas Geoscience, 2012, 23(4): 607-615.]
[10]	童晓光,郭彬程,李建忠,等. 中美致密砂岩气成藏分布异同点比较研究与意义[J]. 中国工程科学,2012,14(6): 9-15.[Tong Xiaoguang, Guo Bincheng, Li Jianzhong, et al. Comparison study on accumulation & distribution of tight sandstone gas between China and the United States and its significance[J]. Engineering Sciences, 2012, 14(6): 9-15.]
[11]	张国生,赵文智,杨涛,等. 我国致密砂岩气资源潜力、分布与未来发展地位[J]. 中国工程科学,2012,14(6):87-93.[Zhang Guosheng, Zhao Wenzhi, Yang Tao, et al. Resource evaluation,position and distribution of tight sandstone gas in China[J]. Engineering Sciences, 2012, 14(6): 87-93.]
[12]	何登发,周新源,杨海军,等. 库车坳陷的地质结构及其对大油气田的控制作用[J]. 大地构造与成矿学,2009,33(1):19-32.[He Dengfa, Zhou Xinyuan, Yang Haijun, et al. Geological structure and its controls on giant oil and gas fields in Kuqa depression, Tarim Basin: A clue from new shot seismic data[J].Geotectonica et Metallogenia, 2009, 33(1): 19-32.]
[13]	贾进华,薛良清. 库车坳陷中生界陆相层序地层格架与盆地演化[J]. 地质科学,2002,37(增刊):121-128.[Jia Jinhua, Xue Liangqing. Pattern and evolution of Mesozoic continental sequence stratigraphy in the Kuqa depression[J]. Chinese Journal of Geology, 2002, 37(Suppl.): 121-128.]
[14]	卢双舫,赵孟军,付广,等. 塔里木盆地库车油气系统富气的主控因素分析[J]. 大庆石油学院学报,2001,25(3):10-13.[Lu Shuangfang, Zhao Mengjun, Fu Guan, et al. Key factor analysis of enriching in natural gas in Kuche petroleum system, Tarim Basin[J]. Journal of Daqing Petroleum Institute, 2001, 25(3): 10-13.]
[15]	吕锡敏,皮学军,任战利,等. 库车前陆盆地含油气系统的地质特征[J]. 天然气地球科学,2004,15(3):214-217.[Lü Ximin, Pi Xuejun, Ren Zhanli, et al. The geological characteristics of the petroleum system in Kucha Foreland Basin[J]. Natural Gas Geoscience, 2004, 15(3): 214-217.]
[16]	杨申谷,邹华耀. 依南构造下侏罗统储层影响因素分析[J]. 河南石油,2004,18(4):4-6.[Yang Shengu, Zou Huayao. An analysis of influential factors on Lower Jurassic reservoirs in Yinan Structure[J]. Henan Petroleum, 2004, 18(4): 4-6.]
[17]	孙先达,索丽敏,张民志,等. 激光共聚焦扫描显微检测技术在大庆探区储层分析研究中的新进展[J]. 岩石学报,2005,21(5):1479-1488.[Sun Xianda, Suo Limin, Zhang Minzhi,et al. New progress of reservoir research by the technology of laser confocal scanning microscope analysis in the Daqing exploration area[J]. Acta Petrologica Sinica, 2005, 21(5): 1479-1488.]
[18]	应凤祥,杨式升,张敏,等. 激光扫描共聚焦显微镜研究储层孔隙结构[J]. 沉积学报,2002,20(1):75-79.[Ying Fengxiang, Yang Shisheng, Zhang Min, et al. Application of laser scanning confocal microscope to the measurement of pore texture in reservoirs[J]. Acta Sedimentologica Sinica, 2002, 20(1): 75-79.]
[19]	白玉彬,赵靖舟,方朝强,等. 鄂尔多斯盆地长6油层组准连续型致密砂岩油藏形成机理[J]. 石油实验地质,2013,35(1):65-71.[Bai Yubin, Zhao Jingzhou, Fang Chaoqiang, et al. Forming mechanism of quasi-continuous tight sandstone reservoir of Chang 6 oil-bearing formation,Ordos Basin[J].Petroleum Geology & Experiment, 2013, 35(1): 65-71.]
[20]	赵靖舟,付金华,姚泾利,等. 鄂尔多斯盆地准连续型致密砂岩大气田成藏模式[J]. 石油学报,2012,33(增刊):37-52.[Zhao Jingzhou, Fu Jinhua, Yao Jingli,et al. Quasi-continuous accumulation model of large tight sandstone gas field in Ordos Basin[J]. Acta Petrolei Sinica, 2012, 33(Suppl.): 37-52.]
[21]	Morad S, Al-Ramadan K, Ketzer J M, et al. The impact of diagenesis on the heterogeneity of sandstone reservoirs: A review of the role of depositional facies and sequence stratigraphy [J]. AAPG Bulletin, 2010, 94(8): 1267-1309.
[22]	刘吉余,马志欣,孙淑艳. 致密含气砂岩研究现状及发展展望[J]. 天然气地球科学,2008,19(3):316-319.[Liu Jiyu, Ma Zhixin, Sun Shuyan. Present research situation and prospects of tight gas sands[J]. Natural Gas Geoscience, 2008, 19(3): 316-319.]
[23]	杨升宇,张金川,黄卫东,等. 吐哈盆地柯柯亚地区致密砂岩气储层“甜点”类型及成因[J]. 石油学报,2013,34(2):272-282.[Yang Shengyu, Zhang Jinchuan, Huang Weidong, et al. “Sweet spot” types of reservoirs and genesis of tight sandstone gas in Kekeya area, Turpan-Hami Basin[J]. Acta Petrolei Sinica, 2013, 34(2): 272-282.]
[24]	寿建峰,朱国华,张惠良. 构造侧向挤压与砂岩成岩压实作用——以塔里木盆地为例[J]. 沉积学报,2003,21(1): 90-95.[Shou Jianfeng, Zhu Guohua, Zhang Huiliang. Lateral structure compression and its influence on sandstone diagenesis—A case study from the Tarim Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1): 90-95.]
[25]	杨威,魏国齐,李宇平,等. 库车前陆盆地下侏罗统成岩作用[J]. 天然气工业,2005,25(9):17-19.[Yang Wei, Wei Guoqi, Li Yupin,et al. Diageneses of lower Jurassic in Kuche Foreland Basin[J]. Natural Gas Industry, 2005, 25(9): 17-19.]
[26]	寿建峰,斯春松,朱国华,等. 塔里木盆地库车坳陷下侏罗统砂岩储层性质的控制因素[J]. 地质论评,2001,47(3):272-277.[Shou Jianfeng, Si Chunsong, Zhu Guohua, et al. Controlling factors of the properties of the Lower Jurassic sandstone reservoirs in the Kuqa depression, Tarim Basin[J]. Geological Review, 2001, 47(3): 272-277.]
[27]	杨帆,邸宏利,王少依,等. 塔里木盆地库车坳陷依奇克里克构造带侏罗系储层特征及成因[J]. 古地理学报,2002,4(2):46-55.[Yang Fan, Di Hongli, Wang Shaoyi, et al. Reservoir characteristics and genesis of the Jurassic in Yiqikelike tectonic zone of Kuqa depression in Tarim Basin[J]. Journal of Palaeogeography, 2002, 4(2): 46-55.]
[28]	张荣虎,姚根顺,寿建峰,等. 沉积、成岩、构造一体化孔隙度预测模型[J]. 石油勘探与开发,2011,38(2):145-151.[Zhang Ronghu, Yao Genshun, Shou Jianfeng, et al. An integration porosity forecast model of deposition, diagenesis and structure[J]. Petroleum Exploration and Development, 2011, 38(2): 145-151.]

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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Reservoir Characteristics and Main Controlling Factors of the Lower Jurassic Tight Sandstone in Eastern Kuqa Depression

1. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing 102249;

2. Basin and Reservoir Research Center, China University of Petroleum (Beijing), Beijing 102249

Received Date: 2013-11-18

Rev Recd Date: 2014-05-12

Publish Date: 2015-02-10

Key words:

Abstract: The tight sandstone gas of Tarim Basin has a large distribution and great exploration potential, which is an important prospective exploration field of the basin in the future. The Lower Jurassic sandstone in eastern Kuqa depression is commonly tight. It is important for the further exploration and development to strengthen the study of its reservoir characteristics and the main controlling factors. In order to reveal the controlling factors and development mechanism of the Lower Jurassic tight sandstone reservoir in eastern Kuqa depression, by use of the tests of casting section, cathodeluminescence, scanning electron microscope and laser confocal microscopy are applied, together with the geological and logging analyses. The lithology, pore structure characteristics and physical properties are carried out in this paper. The results show that lithic sandstone is the main reservoir rock type, and the rock composition maturity is low while the textural maturity is of medium degree. The pore structure is mainly mesoporous with fine throat and micropore with fine throat. Majority of the porosity values ranges from 4% to 12%, with an average of 8.12%, and the effective air permeability is mainly (0.1~3)×10^-3μm²; On the basis of the comprehensive analyses of sedimentation, diagenesis and tectonics of tight reservoir strata, the studies suggest that the reservoir physical property is mainly controlled by sedimentation, diagenesis and tectonism. The main controlling factors are granularity and compaction.

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Reference (28)

[1]	Golab A N, Knackstedt M A, Averdunk H,et al. 3D porosity and mineralogy characterization in tight gas sandstones[J]. The Leading Edge, 2010, 29(12): 1476-1483.
[2]	Higgs K E, Zwingmann H, Reyes A G,et al. Diagenesis, porosity evolution, and petroleum emplacement in tight gas reservoirs, Taranaki Basin, New Zealand[J]. Journal of Sedimentary Research, 2007, 77(12): 1003-1025.
[3]	Neves F A, Al-Marzoug A, Kim J J,et al. Fracture characterization of deep tight gas sands using azimuthal velocity and AVO seismic data in Saudi Arabia[J]. The Leading Edge, 2003, 22(5): 469-475.
[4]	Smith T, Sayers C M, Liner C. Introduction to this special section: Tight gas sands[J]. The Leading Edge, 2010, 29(12): 1463.
[5]	Grechka V, Mazumdar P, Shapiro S A. Predicting permeability and gas production of hydraulically fractured tight sands from microseismic data[J]. Geophysics, 2010, 75(1): B1-B10.
[6]	张晓峰,侯明才,陈安清. 鄂尔多斯盆地东北部下石盒子组致密砂岩储层特征及主控因素[J]. 天然气工业,2010,30(11):34-38.[Zhang Xiaofeng, Hou Mingcai, Chen Anqing. Features and main controlling factors of tight sandstone reservoirs in the Lower Shihezi Formation in the northeastern Ordos Basin[J]. Natural Gas Industry, 2010, 30(11): 34-38.]
[7]	张超,李旭平,钟建华,等. 吐哈盆地巴喀油田下侏罗统致密砂岩储层特征及主控因素分析[J]. 山东科技大学学报:自然科学版,2011,30(6):65-72.[Zhang Chao, Li Xuping, Zhong Jianhua,et al. Properties and the main controlling factors of compact sandstone reservoirs in Lower Jurassic series of Baka oilfield in Tuha Basin[J]. Journal of Shandong University of Science and Technology: Natural Science, 2011, 30(6): 65-72.]
[8]	康毅力,罗平亚. 中国致密砂岩气藏勘探开发关键工程技术现状与展望[J]. 石油勘探与开发,2007,34(2):239-245.[Kang Yili, Luo Pingya. Current status and prospect of key techniques for exploration and production of tight sandstone gas reservoirs in China[J]. Petroleum Exploration and Development, 2007, 34(2): 239-245.]
[9]	李建忠,郭彬程,郑民,等. 中国致密砂岩气主要类型、地质特征与资源潜力[J]. 天然气地球科学,2012,23(4):607-615.[Li Jianzhong, Guo Bincheng, Zheng Min, et al. Main type, geological features and resource potential of tight sandstone gas in China[J]. Natural Gas Geoscience, 2012, 23(4): 607-615.]
[10]	童晓光,郭彬程,李建忠,等. 中美致密砂岩气成藏分布异同点比较研究与意义[J]. 中国工程科学,2012,14(6): 9-15.[Tong Xiaoguang, Guo Bincheng, Li Jianzhong, et al. Comparison study on accumulation & distribution of tight sandstone gas between China and the United States and its significance[J]. Engineering Sciences, 2012, 14(6): 9-15.]
[11]	张国生,赵文智,杨涛,等. 我国致密砂岩气资源潜力、分布与未来发展地位[J]. 中国工程科学,2012,14(6):87-93.[Zhang Guosheng, Zhao Wenzhi, Yang Tao, et al. Resource evaluation,position and distribution of tight sandstone gas in China[J]. Engineering Sciences, 2012, 14(6): 87-93.]
[12]	何登发,周新源,杨海军,等. 库车坳陷的地质结构及其对大油气田的控制作用[J]. 大地构造与成矿学,2009,33(1):19-32.[He Dengfa, Zhou Xinyuan, Yang Haijun, et al. Geological structure and its controls on giant oil and gas fields in Kuqa depression, Tarim Basin: A clue from new shot seismic data[J].Geotectonica et Metallogenia, 2009, 33(1): 19-32.]
[13]	贾进华,薛良清. 库车坳陷中生界陆相层序地层格架与盆地演化[J]. 地质科学,2002,37(增刊):121-128.[Jia Jinhua, Xue Liangqing. Pattern and evolution of Mesozoic continental sequence stratigraphy in the Kuqa depression[J]. Chinese Journal of Geology, 2002, 37(Suppl.): 121-128.]
[14]	卢双舫,赵孟军,付广,等. 塔里木盆地库车油气系统富气的主控因素分析[J]. 大庆石油学院学报,2001,25(3):10-13.[Lu Shuangfang, Zhao Mengjun, Fu Guan, et al. Key factor analysis of enriching in natural gas in Kuche petroleum system, Tarim Basin[J]. Journal of Daqing Petroleum Institute, 2001, 25(3): 10-13.]
[15]	吕锡敏,皮学军,任战利,等. 库车前陆盆地含油气系统的地质特征[J]. 天然气地球科学,2004,15(3):214-217.[Lü Ximin, Pi Xuejun, Ren Zhanli, et al. The geological characteristics of the petroleum system in Kucha Foreland Basin[J]. Natural Gas Geoscience, 2004, 15(3): 214-217.]
[16]	杨申谷,邹华耀. 依南构造下侏罗统储层影响因素分析[J]. 河南石油,2004,18(4):4-6.[Yang Shengu, Zou Huayao. An analysis of influential factors on Lower Jurassic reservoirs in Yinan Structure[J]. Henan Petroleum, 2004, 18(4): 4-6.]
[17]	孙先达,索丽敏,张民志,等. 激光共聚焦扫描显微检测技术在大庆探区储层分析研究中的新进展[J]. 岩石学报,2005,21(5):1479-1488.[Sun Xianda, Suo Limin, Zhang Minzhi,et al. New progress of reservoir research by the technology of laser confocal scanning microscope analysis in the Daqing exploration area[J]. Acta Petrologica Sinica, 2005, 21(5): 1479-1488.]
[18]	应凤祥,杨式升,张敏,等. 激光扫描共聚焦显微镜研究储层孔隙结构[J]. 沉积学报,2002,20(1):75-79.[Ying Fengxiang, Yang Shisheng, Zhang Min, et al. Application of laser scanning confocal microscope to the measurement of pore texture in reservoirs[J]. Acta Sedimentologica Sinica, 2002, 20(1): 75-79.]
[19]	白玉彬,赵靖舟,方朝强,等. 鄂尔多斯盆地长6油层组准连续型致密砂岩油藏形成机理[J]. 石油实验地质,2013,35(1):65-71.[Bai Yubin, Zhao Jingzhou, Fang Chaoqiang, et al. Forming mechanism of quasi-continuous tight sandstone reservoir of Chang 6 oil-bearing formation,Ordos Basin[J].Petroleum Geology & Experiment, 2013, 35(1): 65-71.]
[20]	赵靖舟,付金华,姚泾利,等. 鄂尔多斯盆地准连续型致密砂岩大气田成藏模式[J]. 石油学报,2012,33(增刊):37-52.[Zhao Jingzhou, Fu Jinhua, Yao Jingli,et al. Quasi-continuous accumulation model of large tight sandstone gas field in Ordos Basin[J]. Acta Petrolei Sinica, 2012, 33(Suppl.): 37-52.]
[21]	Morad S, Al-Ramadan K, Ketzer J M, et al. The impact of diagenesis on the heterogeneity of sandstone reservoirs: A review of the role of depositional facies and sequence stratigraphy [J]. AAPG Bulletin, 2010, 94(8): 1267-1309.
[22]	刘吉余,马志欣,孙淑艳. 致密含气砂岩研究现状及发展展望[J]. 天然气地球科学,2008,19(3):316-319.[Liu Jiyu, Ma Zhixin, Sun Shuyan. Present research situation and prospects of tight gas sands[J]. Natural Gas Geoscience, 2008, 19(3): 316-319.]
[23]	杨升宇,张金川,黄卫东,等. 吐哈盆地柯柯亚地区致密砂岩气储层“甜点”类型及成因[J]. 石油学报,2013,34(2):272-282.[Yang Shengyu, Zhang Jinchuan, Huang Weidong, et al. “Sweet spot” types of reservoirs and genesis of tight sandstone gas in Kekeya area, Turpan-Hami Basin[J]. Acta Petrolei Sinica, 2013, 34(2): 272-282.]
[24]	寿建峰,朱国华,张惠良. 构造侧向挤压与砂岩成岩压实作用——以塔里木盆地为例[J]. 沉积学报,2003,21(1): 90-95.[Shou Jianfeng, Zhu Guohua, Zhang Huiliang. Lateral structure compression and its influence on sandstone diagenesis—A case study from the Tarim Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1): 90-95.]
[25]	杨威,魏国齐,李宇平,等. 库车前陆盆地下侏罗统成岩作用[J]. 天然气工业,2005,25(9):17-19.[Yang Wei, Wei Guoqi, Li Yupin,et al. Diageneses of lower Jurassic in Kuche Foreland Basin[J]. Natural Gas Industry, 2005, 25(9): 17-19.]
[26]	寿建峰,斯春松,朱国华,等. 塔里木盆地库车坳陷下侏罗统砂岩储层性质的控制因素[J]. 地质论评,2001,47(3):272-277.[Shou Jianfeng, Si Chunsong, Zhu Guohua, et al. Controlling factors of the properties of the Lower Jurassic sandstone reservoirs in the Kuqa depression, Tarim Basin[J]. Geological Review, 2001, 47(3): 272-277.]
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Reservoir Characteristics and Main Controlling Factors of the Lower Jurassic Tight Sandstone in Eastern Kuqa Depression

doi: 10.14027/j.cnki.cjxb.2015.01.017

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通讯作者: 陈斌, bchen63@163.com

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