The Formation Mechanism of Reservoir Differences between the Hanging Wall and the Foot Wall of Ke-Bai Overthrust Fault,Junggar Basin

ZHU ShiFa; LIU Xin; ZHU XiaoMin; WAN Ce; YOU XinCai; JI Lin; DU JianPeng

doi:10.14027/j.cnki.cjxb.2015.01.020

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ZHU ShiFa, LIU Xin, ZHU XiaoMin, WAN Ce, YOU XinCai, JI Lin, DU JianPeng. The Formation Mechanism of Reservoir Differences between the Hanging Wall and the Foot Wall of Ke-Bai Overthrust Fault,Junggar Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 194-201. doi: 10.14027/j.cnki.cjxb.2015.01.020

Citation:

ZHU ShiFa, LIU Xin, ZHU XiaoMin, WAN Ce, YOU XinCai, JI Lin, DU JianPeng. The Formation Mechanism of Reservoir Differences between the Hanging Wall and the Foot Wall of Ke-Bai Overthrust Fault,Junggar Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 194-201. doi: 10.14027/j.cnki.cjxb.2015.01.020

The Formation Mechanism of Reservoir Differences between the Hanging Wall and the Foot Wall of Ke-Bai Overthrust Fault,Junggar Basin

doi: 10.14027/j.cnki.cjxb.2015.01.020

1.
State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249;
2.
College of Geosciences, China University of Petroleum, Beijing 102249;
3.
Xinjiang Oilfield Company, CNPC, Karamay, Xinjiang, 834000

Received Date: 2014-01-09
Rev Recd Date: 2014-05-05
Publish Date: 2015-02-10

Abstract

On the basis of a large number of thin-sections, casting thin-sections, and physical property analysis of cores, the article systematically compares Permian-Jurassic reservoir differences between the foot wall and the hanging wall of the Ke-Bai overthrust fault, northwestern margin of Junggar Basin from the perspectives of structural evolution, time-space distribution of the depositional system, diagenesis evolution, and reservoir quality. The formation mechanism of reservoir differences have been discussed. The reservoir on the hanging wall is near to the provenance with coarse grain size and shallow burial depth. The lithologies are conglomerate and sandy conglomerate of alluvial fan and braided river. The compaction is weak and a large number of primary pores are well preserved. The reservoir on the foot wall is far away from the provenance with deeper burial depth and finer grain size. The lithology is sandstone of braided river delta and fan delta front. Zeolites and feldspars are intensely dissolved within some intervals. Comprehensive analysis shows that the reservoir burial history (fracture evolutionary history) controlled facies association, present burial depth, and the formation of secondary porosity in the study area. Depositional systems effected by Ke-Bai fault had a genetic impact on the grain size, compositional maturity and textural maturity of the reservoir rocks, controlling the development of primary pore configuration.
- Junggar Basin,
- overthrust fault zone,
- reservoir differences,
- formation mechanism

References

[1]	谭开俊,张帆,吴晓智,等. 准噶尔盆地西北缘盆山耦合与油气成藏[J]. 天然气工业,2008,28(5):10-13. [Tan Kaijun, Zhang Fan, Wu Xiaozhi, et al. Basin-range coupling and hydrocarbon accumulation at the northwestern margin of the Junggar Basin[J]. Natural Gas Industry, 2008, 28(5): 10-13.]
[2]	况军,张越迁,侯连华. 准噶尔盆地西北缘克百掩伏带勘探领域分析[J]. 新疆石油地质,2008,29(4):431-434. [Kuang Jun, Zhang Yueqian, Hou Lianhua. Exploratory targets of Karamay-Baikouquan buried structural belt in northwestern margin of Junggar Basin[J]. Xinjiang Petroleum Geology, 2008, 29(4): 431-434.]
[3]	鲁兵,张进,李涛,等. 准噶尔盆地构造格架分析[J]. 新疆石油地质,2008,29(3):283-289. [Lu Bing, Zhang Jin, Li Tao, et al. Analysis of tectonic framework in Junggar Basin[J]. Xinjiang Petroleum Geology, 2008, 29(3): 283-289.]
[4]	Zhu Shifa, Zhu Xiaomin, Liu Jishan,et al. Genesis and hydrocarbon significance of vesicular welded tuffs: A case study from the Fengcheng Formation, Wu-Xia area, Junggar Basin, NW China[J]. Petroleum Exploration and Development, 2012, 39(2): 173-183.
[5]	Harris N B. Reservoir geology of Fangst Group (Middle Jurassic) Heidrun field, offshore mid-Norway[J]. AAPG Bulletin, 1989, 73: 1415-1435.
[6]	Payne J H. Diagenetic variations in the Permo-Triassic Ivishak sandstone in the Prudhoe Bay field and central-northeastern national petroleum reserve in Alaska (NPRA)[C]// Tailleur I, Weimer P. Alaska North Slope geology. SEPM Pacific Section and Alaska Geological Society, 1987: 77-83.
[7]	朱筱敏,张守鹏,韩雪芳,等. 济阳坳陷陡坡带沙河街组砂砾岩体储层质量差异性研究[J]. 沉积学报,2013,31(6):1094-1104. [Zhu Xiaomin, Zhang Shoupeng, Han Xuefang, et al. On the differences of reservoir quality of Shahejie Fm. in steep slope zones of Jiyang sag [J]. Acta Sedimentologica Sinica, 2013, 31(6): 1094-1104.]
[8]	李小陪,高志勇,李书凯,等. 库车前陆盆地上侏罗统—下白垩统砾岩特征与构造演化关系[J]. 沉积学报,2013,31(6):980-993. [Li Xiaopei, Gao Zhiyong, Li Shukai, et al. Relationship between conglomeratic characteristics and tectonic evolution of Upper Jurassic-Lower Cretaceous in Kuqa Foreland Basin [J]. Acta Sedimentologica Sinica, 2013, 31(6): 980-993.]
[9]	Bloch S, McGowen J H, Duncan J R, et al. Porosity prediction, prior to drilling, in sandstones of the Kekiktuk Formation (Mississippian), North Slope of Alaska[J]. AAPG Bulletin, 1990, 74(9): 1371-1385.
[10]	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.]
[11]	邵雨,汪仁富,张越迁,等. 准噶尔盆地西北缘走滑构造与油气勘探[J]. 石油学报,2011,32(6):976-984. [Shao Yu, Wang Renfu, Zhang Yueqian, et al. Strike-slip structures and oil-gas exploration in the NW margin of the Junggar Basin, China[J]. Acta Petrolei Sinica, 2011, 32(6): 976-984.]
[12]	邹才能,侯连华,匡立春,等. 准噶尔盆地西缘二叠—三叠系扇控成岩储集相成因机理[J]. 地质科学,2007,42(3):587-601. [Zou Caineng, Hou Lianhua, Kuang Lichun, et al. Genetic mechanism of diagenesis-reservoir facies of the fan-controlled Permo-Triassic in the western marginal area, Junggar Basin[J]. Chinese Journal of Geology, 2007, 42(3): 587-601.]
[13]	何登发,尹成,杜社宽,等. 前陆冲断带构造分段特征——以准噶尔盆地西北缘断裂构造带为例[J]. 地学前缘,2004,11(3):91-101. [He Dengfa, Yin Cheng, Du Shekuan, et al. Characteristics of structural segmentation of foreland thrust belts—A case study of the fault belts in the northwestern margin of Junggar Basin[J]. Earth Science Frontiers, 2004, 11(3): 91-101.]
[14]	陈书平,况军,刘继山,等. 准噶尔盆地西北缘克—百地区不整合面及其动力学条件[J]. 高校地质学报,2008,14(2):199-205. [Chen Shuping, Kuang Jun, Liu Jishan, et al. Major unconformities and their dynamic conditions in Ke-Bai area, northwestern margin of Junggar Basin[J]. Geological Journal of China Universities, 2008, 14(2):199-205.]
[15]	雷振宇,鲁兵,蔚远江,等. 准噶尔盆地西北缘构造演化与扇体形成和分布[J]. 石油与天然气地质,2005,26(1):86-91. [Lei Zhenyu, Lu Bing, Wei Yuanjiang, et al. Tectonic evolution and development and distribution of fans on northwestern edge of Junggar Basin[J]. Oil & Gas Geology, 2005, 26(1): 86-91.]
[16]	雷振宇,卞德智,杜社宽,等. 准噶尔盆地西北缘扇体形成特征及油气分布规律[J]. 石油学报,2005,26(1):8-12. [Lei Zhenyu, Bian Dezhi, Du Shekuan, et al. Characteristics of fan forming and oil-gas distribution in west-north margin of Junggar Basin[J]. Acta Petrolei Sinica, 2005, 26(1): 8-12.]
[17]	朱世发. 混积地层储层发育机理和主控因素分析——以准噶尔盆地乌—夏地区二叠系风城组为例[D]. 北京:中国石油大学(北京),2011.[Zhu Shifa. Genetic mechanism and main controlling factors of reservoir rocks in mixed formations - A case study in the Fengcheng Formation of Permian in Wu-Xia area, Junggar Basin[D]. Beijing: China University of Petroleum, Beijing, 2011.]
[18]	丘东洲,张继庆,王熙林,等. 准噶尔盆地西北缘三叠—侏罗系储层沉积成岩与评价[M]. 成都:成都科技大学出版社,1994. [Qiu Dongzhou, Zhang Jiqing, Wang Xilin, et al. Triassic -Jurassic Reservoir Deposition and Diagenesis in Northwestern Margin, Junggar Basin[M]. Chengdu: Chengdu University of Science and Technology Press, 1994.]
[19]	Zhang Jinliang, Jia Ying, Du Guilin. Diagenesis and its effect on reservoir quality of Silurian sandstones, Tabei area, Tarim Basin, China[J]. Petroleum Science, 2007, 4(3): 1-13.
[20]	Zhu Xiaomin, Zhong Dakang, Zhang Qin,et al. Sandstone diagenesis and porosity evolution of Paleogene in Huimin Depression[J]. Petroleum Science, 2004, 1(3): 23-29.
[21]	朱世发,朱筱敏,刘振宇,等. 准噶尔盆地西北缘克—百地区侏罗系成岩作用及其对储层质量的影响[J]. 高校地质学报,2008,14(2):172-180. [Zhu Shifa, Zhu Xiaomin, Liu Zhenyu, et al. Jurassic diagenesis and its control on reservoir quality in Ke-Bai area, northwestern margin of Junggar Basin[J]. Geological Journal of China Universities, 2008, 14(2): 172-180.]
[22]	Jiang Zhenxue, Chen Dongxia, Pang Xiongqi,et al. Control of formation of lithological reservoirs by surrounding mudstone[J]. Petroleum Science, 2006, 3(2): 1-6.
[23]	Zhu Shifa, Zhu Xiaomin, Wang Xulong,et al. Zeolite diagenesis and its control on petroleum reservoir quality of Permian in northwestern margin of Junggar Basin, China[J]. Science China Earth Sciences, 2012, 55(3): 386-396.

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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The Formation Mechanism of Reservoir Differences between the Hanging Wall and the Foot Wall of Ke-Bai Overthrust Fault,Junggar Basin

1. State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249;

2. College of Geosciences, China University of Petroleum, Beijing 102249;

3. Xinjiang Oilfield Company, CNPC, Karamay, Xinjiang, 834000

Received Date: 2014-01-09

Rev Recd Date: 2014-05-05

Publish Date: 2015-02-10

Key words:

Abstract: On the basis of a large number of thin-sections, casting thin-sections, and physical property analysis of cores, the article systematically compares Permian-Jurassic reservoir differences between the foot wall and the hanging wall of the Ke-Bai overthrust fault, northwestern margin of Junggar Basin from the perspectives of structural evolution, time-space distribution of the depositional system, diagenesis evolution, and reservoir quality. The formation mechanism of reservoir differences have been discussed. The reservoir on the hanging wall is near to the provenance with coarse grain size and shallow burial depth. The lithologies are conglomerate and sandy conglomerate of alluvial fan and braided river. The compaction is weak and a large number of primary pores are well preserved. The reservoir on the foot wall is far away from the provenance with deeper burial depth and finer grain size. The lithology is sandstone of braided river delta and fan delta front. Zeolites and feldspars are intensely dissolved within some intervals. Comprehensive analysis shows that the reservoir burial history (fracture evolutionary history) controlled facies association, present burial depth, and the formation of secondary porosity in the study area. Depositional systems effected by Ke-Bai fault had a genetic impact on the grain size, compositional maturity and textural maturity of the reservoir rocks, controlling the development of primary pore configuration.

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Reference (23)

[1]	谭开俊,张帆,吴晓智,等. 准噶尔盆地西北缘盆山耦合与油气成藏[J]. 天然气工业,2008,28(5):10-13. [Tan Kaijun, Zhang Fan, Wu Xiaozhi, et al. Basin-range coupling and hydrocarbon accumulation at the northwestern margin of the Junggar Basin[J]. Natural Gas Industry, 2008, 28(5): 10-13.]
[2]	况军,张越迁,侯连华. 准噶尔盆地西北缘克百掩伏带勘探领域分析[J]. 新疆石油地质,2008,29(4):431-434. [Kuang Jun, Zhang Yueqian, Hou Lianhua. Exploratory targets of Karamay-Baikouquan buried structural belt in northwestern margin of Junggar Basin[J]. Xinjiang Petroleum Geology, 2008, 29(4): 431-434.]
[3]	鲁兵,张进,李涛,等. 准噶尔盆地构造格架分析[J]. 新疆石油地质,2008,29(3):283-289. [Lu Bing, Zhang Jin, Li Tao, et al. Analysis of tectonic framework in Junggar Basin[J]. Xinjiang Petroleum Geology, 2008, 29(3): 283-289.]
[4]	Zhu Shifa, Zhu Xiaomin, Liu Jishan,et al. Genesis and hydrocarbon significance of vesicular welded tuffs: A case study from the Fengcheng Formation, Wu-Xia area, Junggar Basin, NW China[J]. Petroleum Exploration and Development, 2012, 39(2): 173-183.
[5]	Harris N B. Reservoir geology of Fangst Group (Middle Jurassic) Heidrun field, offshore mid-Norway[J]. AAPG Bulletin, 1989, 73: 1415-1435.
[6]	Payne J H. Diagenetic variations in the Permo-Triassic Ivishak sandstone in the Prudhoe Bay field and central-northeastern national petroleum reserve in Alaska (NPRA)[C]// Tailleur I, Weimer P. Alaska North Slope geology. SEPM Pacific Section and Alaska Geological Society, 1987: 77-83.
[7]	朱筱敏,张守鹏,韩雪芳,等. 济阳坳陷陡坡带沙河街组砂砾岩体储层质量差异性研究[J]. 沉积学报,2013,31(6):1094-1104. [Zhu Xiaomin, Zhang Shoupeng, Han Xuefang, et al. On the differences of reservoir quality of Shahejie Fm. in steep slope zones of Jiyang sag [J]. Acta Sedimentologica Sinica, 2013, 31(6): 1094-1104.]
[8]	李小陪,高志勇,李书凯,等. 库车前陆盆地上侏罗统—下白垩统砾岩特征与构造演化关系[J]. 沉积学报,2013,31(6):980-993. [Li Xiaopei, Gao Zhiyong, Li Shukai, et al. Relationship between conglomeratic characteristics and tectonic evolution of Upper Jurassic-Lower Cretaceous in Kuqa Foreland Basin [J]. Acta Sedimentologica Sinica, 2013, 31(6): 980-993.]
[9]	Bloch S, McGowen J H, Duncan J R, et al. Porosity prediction, prior to drilling, in sandstones of the Kekiktuk Formation (Mississippian), North Slope of Alaska[J]. AAPG Bulletin, 1990, 74(9): 1371-1385.
[10]	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.]
[11]	邵雨,汪仁富,张越迁,等. 准噶尔盆地西北缘走滑构造与油气勘探[J]. 石油学报,2011,32(6):976-984. [Shao Yu, Wang Renfu, Zhang Yueqian, et al. Strike-slip structures and oil-gas exploration in the NW margin of the Junggar Basin, China[J]. Acta Petrolei Sinica, 2011, 32(6): 976-984.]
[12]	邹才能,侯连华,匡立春,等. 准噶尔盆地西缘二叠—三叠系扇控成岩储集相成因机理[J]. 地质科学,2007,42(3):587-601. [Zou Caineng, Hou Lianhua, Kuang Lichun, et al. Genetic mechanism of diagenesis-reservoir facies of the fan-controlled Permo-Triassic in the western marginal area, Junggar Basin[J]. Chinese Journal of Geology, 2007, 42(3): 587-601.]
[13]	何登发,尹成,杜社宽,等. 前陆冲断带构造分段特征——以准噶尔盆地西北缘断裂构造带为例[J]. 地学前缘,2004,11(3):91-101. [He Dengfa, Yin Cheng, Du Shekuan, et al. Characteristics of structural segmentation of foreland thrust belts—A case study of the fault belts in the northwestern margin of Junggar Basin[J]. Earth Science Frontiers, 2004, 11(3): 91-101.]
[14]	陈书平,况军,刘继山,等. 准噶尔盆地西北缘克—百地区不整合面及其动力学条件[J]. 高校地质学报,2008,14(2):199-205. [Chen Shuping, Kuang Jun, Liu Jishan, et al. Major unconformities and their dynamic conditions in Ke-Bai area, northwestern margin of Junggar Basin[J]. Geological Journal of China Universities, 2008, 14(2):199-205.]
[15]	雷振宇,鲁兵,蔚远江,等. 准噶尔盆地西北缘构造演化与扇体形成和分布[J]. 石油与天然气地质,2005,26(1):86-91. [Lei Zhenyu, Lu Bing, Wei Yuanjiang, et al. Tectonic evolution and development and distribution of fans on northwestern edge of Junggar Basin[J]. Oil & Gas Geology, 2005, 26(1): 86-91.]
[16]	雷振宇,卞德智,杜社宽,等. 准噶尔盆地西北缘扇体形成特征及油气分布规律[J]. 石油学报,2005,26(1):8-12. [Lei Zhenyu, Bian Dezhi, Du Shekuan, et al. Characteristics of fan forming and oil-gas distribution in west-north margin of Junggar Basin[J]. Acta Petrolei Sinica, 2005, 26(1): 8-12.]
[17]	朱世发. 混积地层储层发育机理和主控因素分析——以准噶尔盆地乌—夏地区二叠系风城组为例[D]. 北京:中国石油大学(北京),2011.[Zhu Shifa. Genetic mechanism and main controlling factors of reservoir rocks in mixed formations - A case study in the Fengcheng Formation of Permian in Wu-Xia area, Junggar Basin[D]. Beijing: China University of Petroleum, Beijing, 2011.]
[18]	丘东洲,张继庆,王熙林,等. 准噶尔盆地西北缘三叠—侏罗系储层沉积成岩与评价[M]. 成都:成都科技大学出版社,1994. [Qiu Dongzhou, Zhang Jiqing, Wang Xilin, et al. Triassic -Jurassic Reservoir Deposition and Diagenesis in Northwestern Margin, Junggar Basin[M]. Chengdu: Chengdu University of Science and Technology Press, 1994.]
[19]	Zhang Jinliang, Jia Ying, Du Guilin. Diagenesis and its effect on reservoir quality of Silurian sandstones, Tabei area, Tarim Basin, China[J]. Petroleum Science, 2007, 4(3): 1-13.
[20]	Zhu Xiaomin, Zhong Dakang, Zhang Qin,et al. Sandstone diagenesis and porosity evolution of Paleogene in Huimin Depression[J]. Petroleum Science, 2004, 1(3): 23-29.
[21]	朱世发,朱筱敏,刘振宇,等. 准噶尔盆地西北缘克—百地区侏罗系成岩作用及其对储层质量的影响[J]. 高校地质学报,2008,14(2):172-180. [Zhu Shifa, Zhu Xiaomin, Liu Zhenyu, et al. Jurassic diagenesis and its control on reservoir quality in Ke-Bai area, northwestern margin of Junggar Basin[J]. Geological Journal of China Universities, 2008, 14(2): 172-180.]
[22]	Jiang Zhenxue, Chen Dongxia, Pang Xiongqi,et al. Control of formation of lithological reservoirs by surrounding mudstone[J]. Petroleum Science, 2006, 3(2): 1-6.
[23]	Zhu Shifa, Zhu Xiaomin, Wang Xulong,et al. Zeolite diagenesis and its control on petroleum reservoir quality of Permian in northwestern margin of Junggar Basin, China[J]. Science China Earth Sciences, 2012, 55(3): 386-396.

The Formation Mechanism of Reservoir Differences between the Hanging Wall and the Foot Wall of Ke-Bai Overthrust Fault,Junggar Basin

doi: 10.14027/j.cnki.cjxb.2015.01.020

Abstract

References

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通讯作者: 陈斌, bchen63@163.com

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