蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据

doi:10.7623/syxb201509007

石油学报 ›› 2015, Vol. 36 ›› Issue (9): 1098-1107.DOI: 10.7623/syxb201509007

蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据

白冰, 王清斌, 赵国祥, 刘晓健

中海石油(中国)有限公司天津分公司渤海石油研究院, 天津 300452

收稿日期:2015-03-05 修回日期:2015-07-22 出版日期:2015-09-25 发布日期:2015-09-30
通讯作者: 白冰,男,1986年12月生,2010年获吉林大学地球科学学院学士学位,2013年获吉林大学地球科学学院硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院工程师,主要从事油气勘探及储层研究。Email:baibing3@cnooc.com.cn
作者简介:白冰,男,1986年12月生,2010年获吉林大学地球科学学院学士学位,2013年获吉林大学地球科学学院硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院工程师,主要从事油气勘探及储层研究。Email:baibing3@cnooc.com.cn
基金资助:
国家重大科技专项(2011ZX05023-006)资助。

Cenozoic tectonic evolution of PL9-1 structure: an evidence of apatite fission track

Bai bing, Wang Qingbin, Zhao Guoxiang, Liu Xiaojian

Research Institute of Bohai Oil Field, CNOOC Tianjin Branch Company, Tianjin 300452, China

Received:2015-03-05 Revised:2015-07-22 Online:2015-09-25 Published:2015-09-30

摘要/Abstract

摘要：

作为国内最大的中生界花岗岩潜山油田,蓬莱9-1构造中生界花岗岩的构造演化直接制约着储层的分布及好坏,而区域构造演化证实花岗岩在整个新生代经历了长期的暴露和改造过程。通过磷灰石裂变径迹技术对该构造中生界花岗岩新生代的构造演化进行了详细研究,结果表明该构造新生代热史分为4个降温期和2个升温期共6个阶段,结合区域构造背景可将新生代构造演化进一步划分为稳定期(65~51 Ma)、低速隆升期(51~34 Ma)、高速隆升期(34~18 Ma)、沉降期(18~5 Ma)和成藏期(5 Ma至今)5个阶段。不同隆升期花岗岩剥蚀速率存在明显差异,其高速隆升期剥蚀速率可达110.7 m/Ma,新生代平均剥蚀量约2 260 m。成藏研究证实构造演化与花岗岩成储成藏有着密切联系,隆升期的风化壳形成和沉降期的泥岩沉积使花岗岩具备了良好的储盖组合,成藏期的新构造运动又为油气的运移和充注提供了有利条件。

关键词: 磷灰石裂变径迹, 构造演化, 剥蚀量恢复, 新生代, 蓬莱9-1构造

Abstract:

PL9-1 structure is the largest Mesozoic granite buried-hill oil field in China, where the distribution and quality of reservoirs are directly restricted by tectonic evolution of Mesozoic granites. Regional tectonic evolution has proved that the granites had undergone a long period of exposure and transformation during the whole Cenozoic era. With the use of apatite fission track technology, a detailed research was conducted on the Cenozoic tectonic evolution of Mesozoic granites in PL9-1 structure. The results show that Cenozoic thermal history of PL9-1 structure can be divided into 6 stages, including 4 cooling stages and 2 heating stages. In combination with regional tectonic settings, the Cenozoic tectonic evolution can be further divided into 5 stages, i.e., stable stage (65-51 Ma), low-rate uplift stage (51-34 Ma), high-rate uplift stage (34-18 Ma), sedimentary stage (18-5 Ma) and accumulation stage (5 Ma-present). Denudation rates are significantly different during various uplift stages. The denudation rate can reach 110.7 m/Ma in the high-rate uplift stage, and the average Cenozoic denudation thickness is about 2 260 m. Verified by relevant researches, there is a close relationship between tectonic evolution and granite reservoir accumulation. Granites have a favorable reservoir-cap assemblage due to the formation of weathering crust in the uplift stage and mudstone sedimentation in the sedimentary stage. Meanwhile, the neotectonism in the accumulation stage provides advantages for hydrocarbon migration and filling.

Key words: apatite fission track, tectonic evolution, denudation thickness recovery, Cenozoic era, PL9-1 structure

中图分类号:

TE122.2

白冰, 王清斌, 赵国祥, 刘晓健. 蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据[J]. 石油学报, 2015, 36(9): 1098-1107.

Bai bing, Wang Qingbin, Zhao Guoxiang, Liu Xiaojian. Cenozoic tectonic evolution of PL9-1 structure: an evidence of apatite fission track[J]. Acta Petrolei Sinica, 2015, 36(9): 1098-1107.

参考文献

[1] Landes K K,Amoruso J J,Charlesworth Jr L J,et al.Petroleum resources in basement rocks[J].AAPG Bulletin,1960,44(10):1682-16911.
[2] Pan C H.Petroleum in basement rocks[J].AAPG Bulletin,1982,66(10):1597-1643.
[3] 马龙,刘全新,张景廉,等.论基岩油气藏的勘探前景[J].天然气工业,2006,26(1):8-11.
Ma Long,Liu Quanxin,Zhang Jinglian,et al.A discussion of exploration potentials of basement hydrocarbon reservoir[J].Natural Gas Industry,2006,26(1):8-11.
[4] 邹才能,赵文智,贾承造,等.中国沉积盆地火山岩油气藏形成与分布[J].石油勘探与开发,2008,35(3):257-271.
Zou Caineng,Zhao Wenzhi,Jia Chengzao,et al.Formation and distribution of volcanic hydrocarbon reservoirs in sedimentary basins of China[J].Petroleum Exploration and Development,2008,35(3):257-271.
[5] 高有峰,吴艳辉,刘万洙,等.松辽盆地南部英台断陷营城组火山岩晶间微孔特征及储层效应[J].石油学报, 2013,34(4):667-674.
Gao Youfeng,Wu Yanhui,Liu Wanzhu,et al.Intercrystalline micropore characteristics and reservoir effect of Yingcheng Formation volcanic rock in Yingtai fault depression,southern Songliao Basin[J].Acta Petrolei Sinica,2013,34(4):667-674.
[6] 王岩泉,胡大千,蔡国刚,等.辽河盆地东部凹陷火山岩储层特征与主控因素[J].石油学报,2013,34(5):896-904.
Wang Yanquan,Hu Daqian,Cai Guogang,et al.Characteristics and controlling factors of Cenozoic volcanic reservoirs in Liaohe Basin,NE China[J].Acta Petrolei Sinica,2013,34(5):896-904.
[7] 邓运华.渤海二次勘探成效分析[J].中国海上油气, 2005,17(3):145-147.
Deng Yunhua.An result analysis for the second round of petroleum exploration in Bohai Bay[J].China Offshore Oil and Gas,2005,17(3):145-147.
[8] 李欣,闫伟鹏,崔周旗,等.渤海湾盆地潜山油气藏勘探潜力与方向[J].石油实验地质,2012,34(2):140-144.
Li Xin,Yan Weipeng,Cui Zhouqi,et al.Prospecting potential and targets of buried-hill oil and gas reservoirs in Bohai Bay Basin[J].Petroleum Geology & Experiment,2012,34(2):140-144.
[9] 夏庆龙,周心怀,王昕,等.渤海蓬莱9-1大型复合油田地质特征与发现意义[J].石油学报,2013,34(增刊2):15-23.
Xia Qinglong,Zhou Xinhuai,Wang Xin,et al.Geological characteristics and discovery significance of large-scale and compound oilfield of Penglai 9-1 in Bohai[J].Acta Petrolei Sinica, 2013,34(S2):15-23.
[10] 龚再升.继续勘探中国近海盆地花岗岩储层油气藏[J].中国海上油气,2010,22(4):213-220.
Gong Zaisheng.Continued exploration of granitic-reservoir hydrocarbon accumulations in China offshore basins[J].China Offshore Oil and Gas,2010,22(4):213-220.
[11] 朱伟林,米立军,高阳东,等.大油气田的发现推动中国海域油气勘探迈向新高峰——2012年中国海域勘探工作回顾[J].中国海上油气,2013,25(1):6-12.
Zhu Weilin,Mi Lijun,Gao Yangdong,et al.The discovery of giant and major fields has given impetus to reaching a new peak in hydrocarbon exploration offshore China:a review of 2012 offshore exploration in China[J].China Offshore Oil and Gas,2013,25(1):6-12.
[12] 向才富,冯志强,庞雄奇,等.松辽盆地晚期热历史及其构造意义:磷灰石裂变径迹(AFT)证据[J].中国科学D辑:地球科学,2007,37(8):1024-1031.
Xiang Caifu,Feng Zhiqiang,Pang Xiongqi,et al.Late stage thermal history of the Songliao Basin and its tectonic implications:evidence from apatite fission track (AFT) analyses[J].Science in China Series D:Earth Sciences,2007,50(10):1479-1487.
[13] 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.
[14] 钟大赉,丁林.青藏高原的隆起过程及其机制探讨[J].中国科学D辑:地球科学,1996,26(4):289-295.
Zhong Dalai,Ding Lin.The discussion of uplift process and mechanism in the Tibetan plateau[J].Science in China:Series D,1996,26(4):289-295.
[15] 任战利.利用磷灰石裂变径迹法研究鄂尔多斯盆地地热史[J].地球物理学报,1995,38(3):339-349.
Ren Zhanli.Thermal history of ordos basin assessed by apatite fission track analysis[J].Acta Geophysica Sinica,1995,38(3):339-349.
[16] 赵孟为.磷灰石裂变径迹分析在恢复盆地沉降抬升史中的应用-以鄂尔多斯盆地为例[J].地球物理学报, 1996,39(增1):238-248.
Zhao Mengwei.The application of apatite fission track analysis to the reconstruction of the subsidence and uplift history of sedimentary basins:a case study from the ordos basin[J].Acta Geophysica Sinica,1996,39(Supplement 1):238-248.
[17] Laslett G M,Green P F,Duddy I R,et al.Thermal annealing of fission tracks in apatite 2.A quantitative analysis[J].Chemical Geology:Isotope Geoscience Section,1987,65(1):1-13.
[18] Corrigan J.Inversion of apatite fission track data for thermal history information[J].Journal of Geophysical Research,1991,96(B6):10347-10360.
[19] Ketcham R A,Donelick R A,Donelick M B.AFT Solve:a program for multi-kinetic modeling of apatite fission-track data[J].Geological Materials Research,2000,2:1-32.
[20] 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,2001,22(2):1-7.
Gong Zaisheng,Wang Guochun.Neotectonism and late hydrocarbon accumulation in Bohai sea[J].Acta Petrolei Sinica,2001,22(2):1-7.
[21] 邓运华.郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J].中国海上油气(地质),2001,15(5):301-305.
Deng Yunhua.Control of the neotectonism along Tancheng-Lujiang fracture zone on hydrocarbon accumulation in the eastern Bohai sea[J].China Offshore Oil and Gas (Geology),2001,15(5):301-305.
[22] 漆家福,张一伟,陆克政,等.渤海湾盆地新生代构造演化[J].石油大学学报:自然科学版,1995,19(增刊):1-6.
Qi Jiafu,Zhang Yiwei,Lu Kezheng,et al.Cenozoic tectonic evolution in Bohai bay basin province[J].Journal of the University of Petroleum,China,1995,19(Supplement 1):1-6.
[23] 龚再升,蔡东升,张功成.郯庐断裂对渤海海域东部油气成藏的控制作用[J].石油学报,2007,28(4):1-10.
Gong Zaisheng,Cai Dongsheng,Zhang Gongcheng.Dominating action of Tanlu Fault on hydrocarbon accumulation in eastern Bohai Sea area[J].Acta Petrolei Sinica,2007,28(4):1-10.
[24] 朱伟林,米立军,龚再升,等.渤海海域油气成藏与勘探[M].北京:科学出版社,2009:53-78.
Zhu Weilin,Mi Lijun,Gong Zaisheng,et al.The oil exploration and accumulation in Bohai Sea area[M].Beijing:Science Press,2009:53-78.
[25] 万桂梅,汤良杰,周心怀,等.郯庐断裂带在渤海海域渤东地区的构造特征[J].石油学报,2009,30(3):342-346.
Wan Guimei,Tang Liangjie,Zhou Xinhuai,et al.Tectonic characteristics of the Tanlu fault zone in Bodong area of Bohai Sea[J].Acta Petrolei Sinica,2009,30(3):342-346.
[26] 万桂梅,周东红,汤良杰.渤海海域郯庐断裂带对油气成藏的控制作用[J].石油与天然气地质,2009,30(4):450-454,461.
Wan Guimei,Zhou Donghong,Tang Liangjie.Control of the Tan-Lu fault zone on hydrocarbon accumulation in the Bohai Sea waters[J].Oil & Gas Geology,2009,30(4):450-454,461.
[27] 田立新,吴国强,张金辉.渤海东部庙西地区隆凹结构的形成及与油气聚集的关系[J].石油实验地质,2014,36(1):56-63.
Tian Lixin,Wu Guoqiang,Zhang Jinhui.Formation of uplifts and sags in Miaoxi area of eastern Bohai Sea and their relationship with hydrocarbon accumulation[J].Petroleum Geology & Experiment,2014,36(1):56-63.
[28] Yuan W M,Carter A,Dong J Q,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.
[29] Bellemans F,De Corte F,Van Den Haute P.Composition of SRM and CN U-doped glasses:significance for their use as thermal neutron fluence monitors in fission track dating.Radiation Measurements,1995,24(2):153-160.
[30] Green P F,Duddy I R,Gleadow A J W,et al.Thermal annealing of fission tracks in apatite:1.A qualitative description[J].Chemical Geology:Isotope Geoscience Section,1986,59:237-253.
[31] Hurford A J,Green P F.The zeta age calibration of fission-track dating[J].Chemical Geology,1983,41:285-317.
[32] Hurford A J.Standardization of fission track dating calibration:recommendation by the Fission Track Working Group of the I.U.G.S.Subcommission on Geochronology[J].Chemical Geology:Isotope Geoscience Section,1990,80(2):171-178.
[33] Hurford A J,Green P F.A users' guide to fission track dating calibration[J].Earth and Planetary Science Letters,1982,59(2):343-354.
[34] Green P F.A new look at statistics in fission-track dating[J].Nuclear Tracks,1981,5(1/2):77-86.
[35] Galbraith R F.On statistical models for fission track counts[J].Journal of the International Association for Mathematical Geology,1981,13(6):471-478.
[36] Green P F.The relationship between track shortening and fission track age reduction in apatite:combined influences of inherent instability,annealing anisotropy,length bias and system calibration[J].Earth and Planetary Science Letters, 1988,89(3/4):335-352.
[37] Crowley K D,Cameron M,Schaefer R I.Experimental studies of annealing of etched fission tracks in fluorapatite[J].Geochimica et Cosmochimica Acta,1991,55(5):1449-1465.
[38] 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.
[39] Wygrala B P.Integrated study of an oil field in the southern Po basin,Northern Italy[J].Berichte Kernforschungsanlage J.lich,1989,2313(B6):1-217.
[40] 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.
[41] Kamp P J J.Green P F.Thermal and tectonic history of selected Taranaki Basin (New Zealand) wells assessed by apatite fission track analysis[J].AAPG Bulletin,1990,74(9):1401-1419.
[42] Pichon X L,Henry P,Goffé B.Uplift of Tibet:From eclogites to granulites——Implications for the Andean Plateau and the Variscan belt[J].Tectonophysics,1997,273(1/2):57-76.
[43] 袁万明,杨志强,张招崇,等.安徽省黄山山体的隆升与剥露[J].中国科学:地球科学,2011,41(10):1435-1443.
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.
[44] 崔之久,杨建强,陈艺鑫.中国花岗岩地貌的类型特征与演化[J].地理学报,2007,62(7):675-690.
Cui Zhijiu,Yang Jianqiang,Chen Yixin.The type and evolution of the granite landforms in China[J].Acta Geographica Sinica,2007,62(7):675-690.
[45] 崔之久,陈艺鑫,杨晓燕.黄山花岗岩地貌特征、分布与演化模式[J].科学通报,2009,54(21):3364-3373.
Cui Zhijiu,Chen Yixin,Yang Xiaoyan.Granite landform characteristics,distribution and evolution patterns in Huangshan Mt.[J].Chinese Science Bulletin,2009,54(23):4487-4499.
[46] 官大勇,王永利,王玉秀,等.渤海海域庙西北洼反转构造特征及其对油气成藏控制作用[J].海洋石油,2012,32(1):18-22.
Guan Dayong,Wang Yongli,Wang Yuxiu,et al.Characteristics of inversion structures and their controls over hydrocarbon accumulation in the northern sag of Miaoxi in Bohai sea[J].Offshore Oil,2012,32(1):18-22.
[47] 龚再升.中国近海新生代盆地至今仍然是油气成藏的活跃期[J].石油学报,2005,26(6):1-6.
Gong Zaisheng.Cenozoic China offshore basins keeping active hydrocarbon accumulation to present[J].Acta Petrolei Sinica,2005,26(6):1-6.

蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据

Cenozoic tectonic evolution of PL9-1 structure: an evidence of apatite fission track

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	马钰凯, 孙永河, 马妍, 姜文亚, 孙旭. 渤海湾盆地歧口凹陷构造演化及断裂带成因[J]. 石油学报, 2020, 41(5): 526-539.
[2]	康琳, 吕丁友, 尚锁贵, 高京华, 张江涛. 辽东湾坳陷新生代构造变形特征及营潍断裂带的表现[J]. 石油学报, 2019, 40(S2): 79-90.
[3]	胡圣标, 龙祖烈, 朱俊章, 胡迪, 黄玉平, 史玉玲, 胡杰. 珠江口盆地地温场特征及构造-热演化[J]. 石油学报, 2019, 40(s1): 178-187.
[4]	鲁雪松, 赵孟军, 陈竹新, 李学义, 胡瀚文, 卓勤功. 准噶尔盆地南缘齐古油田油气成藏再认识及勘探启示[J]. 石油学报, 2019, 40(9): 1045-1058,1115.
[5]	蔡少武, 周东红, 王德英, 张京思, 张震, 李颖. 渤海湾盆地秦南凹陷构造发育特征与有利勘探方向[J]. 石油学报, 2019, 40(5): 532-541.
[6]	汪旭东, 张向涛, 林鹤鸣, 阙晓铭, 贺勇, 贾连凯, 肖张波, 李敏. 珠江口盆地陆丰13洼陷中央背斜带地质构造特征及对油气成藏的控制作用[J]. 石油学报, 2019, 40(1): 56-66.
[7]	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.
[8]	陈红汉, 米立军, 刘妍鷨, 韩晋阳, 孔令涛. 珠江口盆地深水区CO₂成因、分布规律与风险带预测[J]. 石油学报, 2017, 38(2): 119-134.
[9]	赵钊, 赵志刚, 沈怀磊, 杨海长, 曾清波, 纪沫, 蔡露露, 杨东升, 李超. 南海北部超深水区双峰盆地构造演化与油气地质条件[J]. 石油学报, 2016, 37(S1): 47-57.
[10]	陈东旭, 章凤奇, 陈汉林, 杨树锋, 曹婷, 蒙启安. 新生代辉绿岩岩体识别及油气地质意义——以中国东北地区方正断陷为例[J]. 石油学报, 2016, 37(6): 757-767.
[11]	王一博, 张功成, 赵志刚, 谢晓军, 刘世翔, 管红, 董伟, 宋双. 南海边缘海构造旋回对沉积充填的控制——以礼乐盆地新生代沉积为例[J]. 石油学报, 2016, 37(4): 474-482.
[12]	汤国民, 罗群, 庞雄奇, 向才富, 汪立群, 魏浩元. 柴西地区南翼山构造天然气来源及成藏模式[J]. 石油学报, 2015, 36(4): 446-456.
[13]	李江海, 王洪浩, 李维波, 周肖贝. 显生宙全球古板块再造及构造演化[J]. 石油学报, 2014, 35(2): 207-218.
[14]	梅庆华, 何登发, 文竹, 李英强, 李皎. 四川盆地乐山—龙女寺古隆起地质结构及构造演化[J]. 石油学报, 2014, 35(1): 11-25.
[15]	岳军培, 张艳, 沈怀磊, 尤龙, 鲁宝亮, 王璞珺. 华南陆缘地质特征对南海北部盆地基底的约束[J]. 石油学报, 2013, 34(增刊二): 120-128.