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ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.
Citation: ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.

Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area

  • Received Date: 2013-07-05
  • Rev Recd Date: 2013-10-14
  • Publish Date: 2014-10-10
  • Considering the modifications of reservoir property in tectonic compression and volcanic hydrothermal transformation area, according to the outcrop and core data, the experimental analysis, and the well logging information, based on the theory of sandstone dynamic diagenesis, we bring forward this research on the effects of tectonic compression and volcanic hydrothermal transformation in marine sandstone reservoirs. It indicates that clastic particles in Yingmai 35 are obviously more compacted than those in Yingmai 34, the rock porosity is 7%~8% less than the latter. The tectonic compaction in early Hercynian and the volcanic hydrothermal transformation in the late Hercynian had improved the reservoir quality in Yingmai 35. The quartz sandstone reservoirs are obviously affected by the tectonic compression and volcanic hydrothermal transformation. The tectonic compression is controlled by the duration,structural pattern,and the original sedimentary fabric. The volcanic hydrotherm has a zonal influence on the sanstone reservoir quality, influencing area is within the half thickness of the volcanic intrusive, the widely distributed metamorphic mineral is the evidence of the destruction of the reservoir.
  • [1] 贾承造. 中国塔里木盆地构造特征与油气[M]. 北京:石油工业出版社, 1997:232-240[Jia Chengzao. Structure Features and Hydrocarbon in Tarim Basin of China[M]. Beijing: Petroleum Industry Press, 1997: 232-240]
    [2] 刘宝珺, 张锦泉. 沉积成岩作用[M]. 北京:科学出版社, 1992:13-20[Liu Baojun, Zhang Jinquan. Deposition Diagenesis[M]. Beijing: Science Press, 1992: 13-20]
    [3] 寿建峰, 张惠良, 朱国华. 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, Zhang Huiliang, Zhu Guohua. 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]
    [4] 寿建峰, 张惠良, 斯春松, 等. 砂岩动力成岩作用[M]. 北京:石油工业出版社, 2005:1-200[Shou Jianfeng, Zhang Huiliang, Si Chunsong, et al. Sandstone Dynamic Diagenesis[M]. Beijing: Petroleum Industry Press, 2005: 1-200]
    [5] 张凤奇, 王震亮, 范昌育. 库车坳陷构造挤压对流体动力的影响[J]. 石油与天然气地质, 2012, 33(2):208-216[Zhang Fengqi, Wang Zhenliang, Fan Changyu. Effects of tectonic compression on hydrodynamic force in Kuqa depression[J]. Oil & Gas Geology, 2012, 33(2): 208-216]
    [6] 孙雄, 洪汉净, 马宗晋. 构造应力作用下流体运动的动力学分析——构造流体动力学[J]. 地球学报, 1998, 19(2):150-157[Sun Xiong, Hong Hanjing, Ma Zongjin. The influence of structure stress on fluid movement-structure fluid dynamics[J]. Acta Geoscientia Sinica, 1998, 19(2): 150-157]
    [7] 丁原辰, 孙宝珊, 汪西海, 等. 塔里木盆地北部油田古应力的AE法测量[J]. 地质力学学报, 1996, 2(2):18-25[Ding Yuanchen, Sun Baoshan, Wang Xihai, et al. Paleostress in northern Tarim oil field estimated by AE[J]. Journal of Geomechanics, 1996, 2(2): 18-25]
    [8] 熊建华, 施豫琴, 过敏. 构造挤压在川东北地区飞仙关组异常高压中的作用[J]. 矿物岩石, 2010, 30(3):83-88[Xiong Jianhua, Shi Yuqin, Guo Min. Effect of tectonic compression on the abnormal pressure of the Feixianguan formation in the northeast Sichuan[J]. Journal of Mineralogy and Petrology, 2010, 30(3): 83-88]
    [9] 石万忠, 陈红汉, 何生. 库车坳陷构造挤压增压的定量评价及超压成因分析[J]. 石油学报, 2007, 28(6):59-65[Shi Wanzhong, Chen Honghan, He Sheng. Quantitative evaluation on contribution of structural compression to overpressure and analysis on origin of overpressure in Kuqa depression[J]. Acta Petrolei Sinica, 2007, 28(6):59-65]
    [10] 张凤奇, 王震亮, 宋岩, 等. 库车坳陷构造挤压增压定量评价新方[J]法. 中国石油大学学报:自然科学版, 2011, 35(4):1-7[Zhang Fengqi, Wang Zhenliang, Song Yan, et al. New method of quantitative evaluation on pressurization resulted from tectonic compression in Kuqa depression[J]. Journal of China University of Petroleum, 2011, 35(4): 1-7]
    [11] 张凤奇, 王震亮, 宋岩, 等. 库车前陆盆地构造挤压作用下的天然气运聚效应探讨[J]. 地质论评, 2012, 58(2):268-276[Zhang Fengqi, Wang Zhenliang, Song Yan, et al. Study on impact of tectonic compression on natural gas migration and accumulation in Kuqa Foreland Basin[J]. Geological Review, 2012, 58(2): 268-276]
    [12] 王璞, 印长海, 朱如凯, 等. 中基性火山作用喷出物类型、特征与成因[J]. 吉林大学学报:地球科学版, 2010, 40(3):469-481[Wang Pu, Yin Changhai, Zhu Rukai, et al. Classification, description and interpretation of the volcanic products: Ancient and modern example from China[J]. Journal of Jilin University: Earth Science Edition, 2010, 40(3): 469-481]
    [13] 高志勇, 胡永军, 张莉华, 等. 准噶尔南缘前陆盆地白垩纪—新近纪构造挤压作用与储层关系的新表征:镜质体反射率与颗粒填集密度[J]. 中国地质, 2010, 37(5):1336-1352[Gao Zhiyong, Hu Yongjun, Zhang Lihua, et al. The interpretation of the controlling action of Cretaceous to Tertiary tectonic compression on the reservoir in the southern margin of Junggar Basin: vitrinite reflectance and grain packing density[J]. Geology in China, 2010, 37(5): 1336-1352]
    [14] 李义军, 樊爱萍, 李浮萍, 等. 苏里格气田二叠系砂体储集性能及其控制因素[J]. 特种油气藏, 2009, 16(6):12-14[Li Yijun, Fan Aiping, Li Fuping, et al. Reservoir properties and control factors of Permian sands in Sulige gas field, Ordos Basin[J]. Special Oil and Gas Reservoirs, 2009, 16(6): 12-14]
    [15] 李曰俊, 吴根耀, 孟庆龙, 等. 塔里木西部地区古生代断裂活动的方式和机制[J]. 地质科学, 2008, 43(4):727-745[Li Yuejun, Wu Genyao, Meng Qinglong, et al. Active modes and mechanisms of the Paleozoic faultings in western Tarim[J]. Chinese Journal of Geology, 2008, 43 (4): 727-745]
    [16] 杨奕华, 包洪平, 贾亚妮. 鄂尔多斯盆地上古生界砂岩储集层控制因素分析[J]. 古地理学报, 2008, 10(3):25-32[Yang Yihua, Bao Hongping, Jia Yani. Analysis on control factors of sandstone reservoir of the Upper Paleozoic in Ordos Basin[J]. Journal of Palaeogeography, 2008, 10(3):25-32]
    [17] 刘嘉麒, 孟凡超. 火山作用与油气成藏[J]. 天然气工业, 2009, 29(8):1-4[Liu Jiaqi, Meng Fanchao. Hydrocarbon generation, migration and accumulation related to igneous activity[J]. Natural Gas Industry, 2009, 29(8): 1-4]
    [18] 曾小英, 张娟, 刘远洋, 等. 沉积期火山作用对川西坳陷须家河组优质储层的意义[J]. 石油与天然气地质, 2012, 33(1):50-60[Zeng Xiaoying, Zhang Juan, Liu Yuanyang, et al. Significance of syndepositional volcanism to high quality reservoirs in the Xujiahe Formation, the western Sichuan depression[J]. Oil & Gas Geology, 2012, 33(1): 50-60]
    [19] 李军, 邹华耀, 张国常. 川东北地区须家河组致密砂岩气藏异常高压成因[J]. 吉林大学学报:地球科学版, 2012, 42(3):624-633[Li Jun, Zou Huayao, Zhang Guochang. Origin of overpressure tight gas reservoir in the Xujiahe Formation, northeastern Sichuan Basin[J]. Journal of Jilin University: Earth Science Edition, 2012, 42(3): 624-633]
    [20] 郭少斌, 洪克岩. 塔里木盆地志留系—泥盆系层序地层及有利储层分布[J]. 石油学报, 2007, 28(3):44-50[Guo Shaobin, Hong Keyan. Silurian-Devonian sequence stratigraphy and favorable reservoir distribution in Tarim Basin[J]. Acta Petrolei Sinica, 2007, 28(3): 44-50]
    [21] 施振生, 杨威, 郭长敏, 等. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3):401-408[Shi Zhensheng, Yang Wei, Guo Changmin, et al. Depositional sequence and filling response characteristics of Silurian in Tarim basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408]
    [22] 施振生, 朱筱敏, 王贵文, 等. 塔里木盆地志留系遗迹化石组合及其沉积环境[J]. 西安石油大学学报:自然科学版, 2004, 19(4):32-39[Shi Zhensheng, Zhu Xiaomin, Wang Guiwen, et al. Silurian ichnoassemblages of Talimu Basin and their sedimentary environments[J]. Journal of Xi'an Shiyou University: Natural Science Edition, 2004, 19(4): 32-39]
    [23] 张金亮, 张鑫. 塔里木盆地志留系古海洋沉积环境的元素地球化学特征[J]. 中国海洋大学学报, 2006, 36(2):200-208[Zhang Jinliang, Zhang Xin. The element geochemical features of ancient oceanic sedimentary environments in the Silurian Period in the Tarim Basin[J]. Periodical of Ocean University of China, 2006, 36(2): 200-208]
    [24] 钟大康, 朱筱敏, 李树静, 等. 早期碳酸盐胶结作用对砂岩孔隙演化的影响——以塔里木盆地满加尔凹陷志留系砂岩为例[J]. 沉积学报, 2007, 25(6):885-890[Zhong Dakang, Zhu Xiaomin, Li Shujing, et al. Influence of early carbonate cementation on the evolution of sandstones: A case study from Silurian sandstones of Manjiaer depression, Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(6): 885-890]
    [25] 刘晓, 关平, 潘文庆, 等. 塔里木盆地二叠系火山岩空间展布的精细刻画及其地质意义[J]. 北京大学学报:自然科学版, 2011, 47(2):314-320[Liu Xiao, Guan Ping, Pan Wenqing, et al. Meticulous characterization of Permian volcanic rocks spatial distribution and its geological significance in the Tarim Basin[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2011, 47(2): 314-320]
    [26] 上官时迈, 田伟, 徐义刚, 等. 塔里木溢流玄武岩的喷发特征[J]. 岩石学报, 2012, 28(4):1261-1272[Shangguan Shimai, Tian Wei, Xu Yigang, et al. The eruption characteristics of the Tarim flood basalt[J]. Acta Petrologica Sinica, 2012, 28(4): 1261-1272]
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  • Received:  2013-07-05
  • Revised:  2013-10-14
  • Published:  2014-10-10

Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area

Abstract: Considering the modifications of reservoir property in tectonic compression and volcanic hydrothermal transformation area, according to the outcrop and core data, the experimental analysis, and the well logging information, based on the theory of sandstone dynamic diagenesis, we bring forward this research on the effects of tectonic compression and volcanic hydrothermal transformation in marine sandstone reservoirs. It indicates that clastic particles in Yingmai 35 are obviously more compacted than those in Yingmai 34, the rock porosity is 7%~8% less than the latter. The tectonic compaction in early Hercynian and the volcanic hydrothermal transformation in the late Hercynian had improved the reservoir quality in Yingmai 35. The quartz sandstone reservoirs are obviously affected by the tectonic compression and volcanic hydrothermal transformation. The tectonic compression is controlled by the duration,structural pattern,and the original sedimentary fabric. The volcanic hydrotherm has a zonal influence on the sanstone reservoir quality, influencing area is within the half thickness of the volcanic intrusive, the widely distributed metamorphic mineral is the evidence of the destruction of the reservoir.

ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.
Citation: ZHANG Rong-Hu, ZHANG Hui-Liang, ZHOU Chen-Guang, SHEN Yang, SHOU Jian-Feng, WANG Bo. Tectonic Compression and Volcanic Hydrothermal Reconstruction Effects of Silurian Sandstone Reservoirs in Yingmaili Area[J]. Acta Sedimentologica Sinica, 2014, 32(5): 901-911.
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