准噶尔盆地中拐地区石炭—二叠纪火山岩特征及构造环境分析
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摘要
中拐地区位于准噶尔盆地西北缘,是在石炭纪—早二叠世挤压应力场作用下形成的宽缓鼻状古隆起。石炭—二叠纪火山岩是主要的含油层系之一,到目前为止已发现了多个油气藏和出油气点,显示出良好的勘探前景。根据系统、精细的地震资料解释,中拐地区在石炭—二叠纪时期主要存在4期构造运动,分别对应4个不整合面:1)石炭系与二叠系之间;2)二叠系佳木河组与下乌尔禾组之间;3)二叠系下乌尔禾组与上乌尔禾组之间;4)二叠系上乌尔禾组与三叠系百口泉组之间。通过对中拐地区石炭—二叠纪火山岩的全岩元素分析表明,该区域主要为中-酸性的安山岩、英安岩和流纹岩及火山角砾岩和凝灰岩为主,其中SiO_2的含量普遍较高,平均含量达到了67%,判定中拐地区的石炭—二叠纪火山岩喷发环境应位于岛弧体系的大陆内侧,在喷发过程中经历过陆壳的熔融作用。结合前人对周缘火山岩的研究,认为石炭—二叠纪时期中拐地区由岛弧环境逐渐进入陆内演化阶段,三叠纪开始进入稳定的沉积演化时期。
Zhong-Guai area is located in the Northwest margin of Junggar Basin,it is a broad nose palaeohigh formed in compressional stress field of Carboniferous Early Permain Period. Carboniferous-Permain volcanic rock is one of the mainly oil-bearing series,until now many hydrocarbon reservoirs and oil entry points are discovered,and showing good exploration prospects.According to systematic and elaborate seismic data interpretation,Zhong-Guai area have four tectonic movements in the Carboniferous-Permian period,corresponding to four unconformity respectively:1 ) Between the Carboniferous and Permian system;2 ) Between the Jiamuhe and Xiawuerhe Formation of Permian system;3 ) Between the Xiawuerhe and Shangwuerhe Formation of Permian system;4 ) Between the Xiawuerhe Formation of Permian system and Baikouquan Formation of Triassic system.The rock element analysis shows that the research area are mainly neutral-acidic andesites,quartz andesite,rhyolite,volcanic breccia and tuff,the content of SiO_2 are generally high,the average content is 66.840%.It is considered that the volcanic eruption environment of Carboniferous-Permain system in research area is inside mainland of island arc system,in the eruption process it experienced the molten role of continental crust.Combining previous study of circumferential volcanic rocks,it is considered that the evolution of Zhong-Guai area in Carboniferous-Permain period is from island arc to intracontinent,and in Triassic period it began to enter into the stable sedimentary evolution period.
Zhong-Guai area is located in the Northwest margin of Junggar Basin,it is a broad nose palaeohigh formed in compressional stress field of Carboniferous Early Permain Period. Carboniferous-Permain volcanic rock is one of the mainly oil-bearing series,until now many hydrocarbon reservoirs and oil entry points are discovered,and showing good exploration prospects.According to systematic and elaborate seismic data interpretation,Zhong-Guai area have four tectonic movements in the Carboniferous-Permian period,corresponding to four unconformity respectively:1 ) Between the Carboniferous and Permian system;2 ) Between the Jiamuhe and Xiawuerhe Formation of Permian system;3 ) Between the Xiawuerhe and Shangwuerhe Formation of Permian system;4 ) Between the Xiawuerhe Formation of Permian system and Baikouquan Formation of Triassic system.The rock element analysis shows that the research area are mainly neutral-acidic andesites,quartz andesite,rhyolite,volcanic breccia and tuff,the content of SiO_2 are generally high,the average content is 66.840%.It is considered that the volcanic eruption environment of Carboniferous-Permain system in research area is inside mainland of island arc system,in the eruption process it experienced the molten role of continental crust.Combining previous study of circumferential volcanic rocks,it is considered that the evolution of Zhong-Guai area in Carboniferous-Permain period is from island arc to intracontinent,and in Triassic period it began to enter into the stable sedimentary evolution period.
引文
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Chen Yequan and Wang Weifeng.2004.Geodynamics process in the Junggar Basin.Journal of Geomechanics,10(2):155- 164.
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Chen Xin,Lu Huafu,Shu Liangshu,Wang Huimin and Zhang Guoqing.2002.Study on tectonic ebolution of Junggar Basin. Geological Journal of China Universities,8(3):257-267.
陈业全,王伟锋.2004.准噶尔盆地构造动力学过程.地质力学学报,10(2):155-164.
Chen Yequan and Wang Weifeng.2004.Geodynamics process in the Junggar Basin.Journal of Geomechanics,10(2):155- 164.
郭召杰,马瑞士,郭令智,施央申.1993.新疆东部三条蛇绿混杂岩带的比较研究.地质评论,39(3):236-247.
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何登发,尹成,杜社宽,石昕,马辉树.2004.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.地学前缘,11(3):91-101.
He Dengfa,Yin Cheng,Du Shekuan,Shi Xin and Ma Huishu.2004.Characteristics of structural segmentation of foreland thrust belts——A case study of the fault belts in the northwestern margin of Junggar Basin.Earth Science Frontiers,11(3): 91-101.
何国琦,韩宝福,岳永君,王嘉桁.1990.中国阿尔泰造山带的构造分区和地壳演化.新疆地质科学,(2):9-20.
He Guoqi,Han Baofu,Yue Yongjun and Wang Jiaheng.1990.Tectonic division and crustal evolution of Altay orogenic belt in China.Xinjiang Journal of Geology,(2):9-20.
侯连华,邹才能,匡立春,王京红,张光亚,况军,刘磊.2009.准噶尔盆地西北缘克—百断裂带石炭系油气成藏控制因素新认识.石油学报,30(4):513-517.
Hou Lianhua,Zou Caineng,Kang Lichun,Wang Jinghong,Zhang Guangya,Kuang Jun and Liu Lei.2009.Discussion on controlling factors for Carboniferous hydrocarbon accumulation in the Ke-Bai fractured zone of the northwestern margin in Junggar Basin.Acta Petrolei Sinica,30(4):513-517.
胡霭琴,王中刚,涂光炽.1997.新疆北部地质演化及成岩成矿规律.北京:科学出版社.78—89.
Hu Aiqin,Wang Zhonggang and Tu Guangchi.1997.Geological Evolution and Feature of Diagenisis and Mineralization of Northern Xinjiang,China.Beijing:Science Press.78—89.
贾承造,何登发,雷振宇,周路,贾进斗,王桂宏.2000.前陆冲断带油气勘探.北京:石油工业出版社,1-351.
Jia Chengzao,He Dengfa,Lei Zhenyu,Zhou Lu,Jia Jindou and Wang Guihong.2000.Oil And Gas Exploration in Foreland Thrust-Folded Belts.Beijing:Petroleum Industry Press.1—351.
况军.2005.准噶尔盆地古隆起与油气勘探方向.新疆石油地质,26(5):502—509.
Kuang Jun.2005.Palaeohighs and targets for petroleumexploration in Jungar Basin.Xinjiang Petroleum Geology,26(5):502—509.
况军,齐雪峰.2006.准噶尔前陆盆地构造特征与油气勘探方向.新疆石油地质,27(1):5—9.
Kuang Jun and Qi Xuefeng.2006.The structural characteristics and oil-gas explorative direction in Junggar foreland basin. Xinjiang Petroleum Geology,27(1 ):5—9.
匡立春,薛新克,邹才能,侯连华.2007.火山岩岩性地层油藏成藏条件与富集规律——以准噶尔盆地克百断裂带上盘石炭系为例.石油勘探与开发,34(3):285—290.
Kuang Lichun,Xue Xinke,Zou Caineng and Hou Lianhua.2007.Oil accumulation and concentration regularity of volcanic lithostratigraphic oil reservoir;A case from upper-plate Carboniferous of Ka-Bai fracture zone,Junggar Basin.Petroleum Exploration and Development,34(3):285—290.
雷振宇,鲁兵,蔚远江,张立平,石昕.2005.准噶尔盆地西北缘构造演化与扇体形成和分布.石油与天然气地质, 26(1):86—91.
Lei Zhenyu.Lu Bing,Wei Yuanjiang,Zhang Liping and Shi Xin.2005.Tectonic evolution and development and distribution of fans on northwestern edge of Junggar Basin.Oil and Gas Geology,26(1 ):86—91.
刘和甫,梁慧社,蔡立国,夏义平,刘立群.1994.天山两侧前陆冲断系构造样式与前陆盆地演化.地球科学,19(6): 727—741.
Liu Hefu,Liang Huishe,Cai Liguo,Xia Yiping and Liu Liqun.1994.Evolution and structural style of Tianshan and adjacent basins,northwestern China.Earth Science,19(6):727—741.
吕锡敏,谭开俊,姚清洲,任培罡,魏东涛,尹路.2006.准噶尔盆地西北缘中拐一五八区二叠系天然气地质特征.天然气地球科学,17(5):708—710.
Lu Ximin,Tan Kaijun,Yao Qingzhou,Ren Peigang,Wei Dongtao and Yin Lu.2006.The geological characteristics of the Permain gas reservoir in Zhongguai-Wubaqu of northwestern margin,Junggar Basin.Natural Gas Geoscience,17(5 ): 708—710.
邵雨,汪仁富,张越迁,汪新,李震华,梁瀚.2011.准噶尔盆地西北缘走滑构造与油气勘探.石油学报,32(6): 976-984.
Shao Yu,Wang Renfu,Zhang Yueqian,Wang Xin,Li Zhenhua and Liang Han.2011.Strike-slip structures and oil-gas exploration in the NW margin of the Junggar Basin,China.Acta Petrolei Sinica,32(6):976—984.
孙国强,姚卫江,张顺存,邢承智,史基安,李兵.2011.准噶尔盆地中拐地区石炭一二叠系火山岩地球化学特征.新疆石油地质,32(6):580—582
Sun Guoqiang,Yao Weijiang,Zhang Shuncun,Xing Chengzhi,Shi Ji'an and Li Bing.2011.Geochemical characteristics of Carboniferous-Permian volcanic rocks in Zhongguai area in northwestern margin of Junggar Basin.Xinjiang Petroleum Geology,32(6):580—582.
涂光炽.1993.新疆北部固体地球科学新进展.北京:科学出版社.15—26.
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