渤海海域辽西凸起北段新生代构造演化的磷灰石裂变径迹证据

doi:10.7623/syxb201811006

石油学报 ›› 2018, Vol. 39 ›› Issue (11): 1262-1271.DOI: 10.7623/syxb201811006

渤海海域辽西凸起北段新生代构造演化的磷灰石裂变径迹证据

张江涛, 吴奎, 王冰洁, 何京, 康琳

中海石油(中国)有限公司天津分公司天津 300459

收稿日期:2018-01-30 修回日期:2018-07-16 出版日期:2018-11-25 发布日期:2018-12-10
通讯作者: 张江涛,男,1988年10月生,2011年获中国石油大学(华东)学士学位,2014年获中国石油大学(华东)硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院勘探地质工程师,主要从事含油气盆地分析等方面的研究。Email:zhangjt28@cnooc.com.cn
作者简介:张江涛,男,1988年10月生,2011年获中国石油大学(华东)学士学位,2014年获中国石油大学(华东)硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院勘探地质工程师,主要从事含油气盆地分析等方面的研究。Email:zhangjt28@cnooc.com.cn
基金资助:
国家科技重大专项（2016ZX05024-002-006）资助。

Apatite fission track evidence of Cenozoic tectonic evolution in the northern section of Liaoxi uplift,Bohai Sea

Zhang Jiangtao, Wu Kui, Wang Bingjie, He Jing, Kang Lin

Tianjin Branch, CNOOC China Limited, Tianjin 300459, China

Received:2018-01-30 Revised:2018-07-16 Online:2018-11-25 Published:2018-12-10

摘要/Abstract

摘要：

通过对辽东湾坳陷辽西凸起北段5块样品的磷灰石裂变径迹测年和热演化史模拟，结合区域地质背景和钻井资料，分析了辽西凸起北段新生代的演化过程。辽西凸起北段在新生代整体发生了大规模的隆升和剥蚀，具有分块性和阶段性抬升剥蚀的特征。西块区存在2个剥蚀期，即65.0~45.8 Ma和25.3~18.6 Ma，平均剥蚀厚度分别为1 737 m和1 020 m；东块区的2个剥蚀期为65.0~36.7 Ma和25.1~19.6 Ma，平均剥蚀厚度分别为1765 m和711 m。辽西凸起北段的新生代构造演化整体划分为6个阶段，但在东、西块区存在明显的差异。新生代构造的时空演化差异主要受控于辽西2号断裂和3号断裂的垂向活动时代和强度。辽西凸起北段西块区的锦州25-1油田经历了2期油气成藏，早成藏期为25.4~24.2 Ma，晚成藏期为10.7~4.5 Ma。

关键词: 磷灰石裂变径迹, 热演化史模拟, 剥蚀量恢复, 构造演化, 辽西凸起北段

Abstract:

Through apatite fission track dating and thermal history simulation of five samples in the northern section of Liaoxi uplift, Liaodong Bay depression, the Cenozoic evolution process of the northern section in Liaoxi uplift was analyzed based on regional geological settings and drilling data. The northern section of Liaoxi uplift presented massive uplift and denudation in Cenozoic, characterized by blocky and phased uplift and denudation. The western block experienced two denudation phases, i.e., 65.0~45.8 Ma and 25.3~18.6 Ma, with the annual denudation thickness of 1737 m and 1020 m; the eastern block experienced two denudation phases of 65.0~36.7 Ma and 25.1~19.6 Ma, with the annual denudation thickness of 1 765 m and 711 m. The Cenozoic tectonic evolution in the northern section of Liaoxi uplift was divided into six stages, and significant differential uplift and decline occurred in the eastern and western blocks. The differences in spatiotemporal evolution of the Cenozoic tectonics were mainly controlled by the vertical activity age and intensity of No.2 and No.3 faults in Liaoxi. Jinzhou 25-1 oilfield in the western block of the northern section in Liaoxi uplift experienced two phases of hydrocarbon accumulation, and the early and late reservoir accumulation phase was 25.4~24.2 Ma and 10.7~4.5 Ma, respectively.

Key words: apatite fission track, thermal history simulation, denudation recovery, tectonic evolution, northern section of Liaoxi uplift

中图分类号:

TE122.2

张江涛, 吴奎, 王冰洁, 何京, 康琳. 渤海海域辽西凸起北段新生代构造演化的磷灰石裂变径迹证据[J]. 石油学报, 2018, 39(11): 1262-1271.

Zhang Jiangtao, Wu Kui, Wang Bingjie, He Jing, Kang Lin. Apatite fission track evidence of Cenozoic tectonic evolution in the northern section of Liaoxi uplift,Bohai Sea[J]. Acta Petrolei Sinica, 2018, 39(11): 1262-1271.

参考文献

[1] 周心怀,刘震,李潍莲.辽东湾断陷油气成藏机理[M].北京:石油工业出社,2009.
ZHOU Xinhuai,LIU Zhen,LI Weilian.Oil and gas accumulation mechanism in Liaodong fault depression[M].Beijing:Petroleum Industry Press,2009.
[2] 余一欣,周心怀,徐长贵,等.渤海海域新生代断裂发育特征及形成机制[J].石油与天然气地质,2011,32(2):273-279.
YU Yixin,ZHOU Xinhuai,XU Changgui,et al.Characteristics and formation mechanisms of the Cenozoic faults in the Bohai Sea waters[J].Oil & Gas Geology,2011,32(2):273-279.
[3] 徐长贵,王冰洁,王飞龙,等.辽东湾坳陷新近系特稠油成藏模式与成藏过程——以旅大5-2北油田为例[J].石油学报,2016,37(5):599-609.
XU Changgui,WANG Bingjie,WANG Feilong,et al.Neogene extra heavy oil accumulation model and process in Liaodong Bay depression:a case study of Lvda 5-2 N oilfield[J].Acta Petrolei Sinica,2016,37(5):599-609.
[4] 胡志伟,徐长贵,杨波,等.渤海海域蓬莱9-1油田花岗岩潜山储层成因机制及石油地质意义[J].石油学报,2017,38(3):274-285.
HU Zhiwei,XU Changgui,YANG Bo,et al.Reservoir forming mechanism of Penglai 9-1 granite buried-hills and its oil geology significance in Bohai Sea[J].Acta Petrolei Sinica,2017,38(3):274-285.
[5] 叶涛,韦阿娟,祝春荣,等.渤海海域基底"改造型火山机构"特征及油气成藏意义[J].石油学报,2016,37(11):1370-1380.
YE Tao,WEI Ajuan,ZHU Chunrong,et al.Characteristics and hydrocarbon accumulation significance of reformed volcanic edifice in the basement of Bohai Sea[J].Acta Petrolei Sinica,2016,37(11):1370-1380.
[6] 龚再升,王国纯.渤海新构造运动控制晚期油气成藏[J].石油学报,2007,22(2):1-7.
GONG Zaisheng,WANG Guochun.Neotectonism and late hydrocarbon accumulation in Bohai Sea[J].Acta Petrolei Sinica,2007,22(2):1-7.
[7] 吴智平,薛雁,颜世永,等.渤海海域渤东地区断裂体系与盆地结构[J].高校地质学报,2013,19(3):463-471.
WU Zhiping,XUE Yan,YAN Shiyong,et al.The development characteristics of the fault system and basin structures of the Bodong sag,East China[J].Geological Journal of China Universities,2013,19(3):463-471.
[8] 贾茹,付晓飞,孟令东,等.断裂及其伴生微构造对不同类型储层的改造机理[J].石油学报,2017,38(3):286-296.
JIA Ru,FU Xiaofei,MENG Lingdong,et al.Transformation mechanism of fault and its associated microstructures for different kinds of reservoirs[J].Acta Petrolei Sinica,2017,38(3):286-296.
[9] 方石,刘招君,黄湘通,等.大兴安岭东南坡新生代隆升及地貌演化的裂变径迹研究[J].吉林大学学报:地球科学版,2008,38(5):771-776.
FANG Shi,LIU Zhaojun,HUANG Xiangtong,et al.Uplift and topography evolution research at FT in cenozoic of south-eastern slope of Daxing'anling mountains[j].Journal of Jilin University:Earth Science Edition,2008,38(5):771-776.
[10] 任健,吴智平,徐长贵,等.辽东凸起北段新生代隆升时间的确定:来自裂变径迹的证据[J].世界地质,2015,34(2):408-418.
REN Jian,WU Zhiping,XU Changgui,et al.Determination of uplifting ages during Cenozoic in northern Liaodong uplift:evidence from fission track dating[J].Global Geology, 2015,34(2):408-418.
[11] 许立青,李三忠,郭玲莉,等.郯庐断裂带对鲁西隆升过程的影响:磷灰石裂变径迹证据[J].岩石学报,2016,32(4):1153-1170.
XU Liqing,LI Sanzhogn,GUO Lingli,et al.Impaction of the Tan-Lu fault zone on uplift of the Luxi rise:constraints from apatite fission track thermochronology[J].Acta Petrologica Sinica,2016,32(4):1153-1170.
[12] 徐长贵,任健,吴智平,等.辽东湾坳陷东部地区新生代断裂体系与构造演化[J].高校地质学报,2015,21(2):215-222.
XU Changgui,REN Jian,WU Zhiping,et al.Cenozoic fault system and tectonic evolution of the eastern liaodong bay depression[J].Geological Journal of China Universities,2015,21(2):215-222.
[13] 彭靖淞,徐长贵,吴奎,等.郯庐断裂带辽东凸起的形成与古辽中洼陷的瓦解[J].石油学报,2015,36(3):274-285.
PENG Jingsong,XU Changgui,WU Kui,et al.Formation of Liaodong uplift and collapse of the ancient Liaozhong sag in Tan-Lu fault zone[J].Acta Petrolei Sinica,2015,36(3):274-285.
[14] GREEN P F.A new look at statistics in fission-track dating[J].Nuclear Tracks,1981,5(1/2):77-86.
[15] GALBRAITH R F.On statistical models for fission track counts[J].Journal of the International Association for Mathematical Geology,1981,13(6):471-478.
[16] YUAN Wanming,CARTER A,DONG Jinquan,et al.Mesozoic-Tertiary exhumation history of the Altai mountains,northern Xinjiang,China:new constraints from apatite fission track data[J].Tectonophysics,2006,412(3/4):183-193.
[17] 周祖翼.低温年代学:原理与应用[M].北京:科学出版社,2014.
ZHOU Zuyi.Low temperature thermochronology:principles & applications[M].Beijing:Science Press,2014.
[18] 邱楠生,魏刚,李翠翠,等.渤海海域现今地温场分布特征[J].石油与天然气地质,2009,30(4):412-419.
QIU Nansheng,WEI Gang,LI Cuicui,et al.Distribution features of current geothermal field in the Bohai Sea waters[J].Oil & Gas Geology,2009,30(4):412-419.
[19] KETCHAM R A,DONELICK R A,CARLSON W D.Variability of apatite fission-track annealing kinetics:Ⅲ.Extrapolation to geological time scales[J].American Mineralogist,1999,84(9):1235-1255.
[20] GALLAGHER K.Evolving temperature histories from apatite fission-track data[J].Earth and Planetary Science Letters,1995,136(3/4):421-435.
[21] GREEN P F,DUDDY I R,BRAY R J.Applications of thermal history reconstruction in inverted basins[M]//BUCHANAN J G,BUCHANAN P G,ed.Basin Inversion.Geological Society of London Special Publication,1995,88:149-165.
[22] YUAN Wanming,YANG Zhiqiang,ZHANG Zhaochong,et al.The uplifting and denudation of main Huangshan mountains,Anhui Province,China[J].Science China Earth Sciences,2011,54(8):1168-1176.

渤海海域辽西凸起北段新生代构造演化的磷灰石裂变径迹证据

Apatite fission track evidence of Cenozoic tectonic evolution in the northern section of Liaoxi uplift,Bohai Sea

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