LA-ICP-MS zircon U-Pb dating of Mesozoic granite in Miaoxibei uplift, Bohai Sea area, and its geological significance

ZHAO Guoxiang; WANG Qingbin; YANG Bo; WANG Feilong; LIU Feng

2017 Vol. 36, No. 7

Article Contents

Article navigation > Geological Bulletin of China > 2017 > 36(7): 1204-1217

Next Article Previous Article

ZHAO Guoxiang, WANG Qingbin, YANG Bo, WANG Feilong, LIU Feng. LA-ICP-MS zircon U-Pb dating of Mesozoic granite in Miaoxibei uplift, Bohai Sea area, and its geological significance[J]. Geological Bulletin of China, 2017, 36(7): 1204-1217.

Citation:

ZHAO Guoxiang, WANG Qingbin, YANG Bo, WANG Feilong, LIU Feng. LA-ICP-MS zircon U-Pb dating of Mesozoic granite in Miaoxibei uplift, Bohai Sea area, and its geological significance[J]. Geological Bulletin of China, 2017, 36(7): 1204-1217.

LA-ICP-MS zircon U-Pb dating of Mesozoic granite in Miaoxibei uplift, Bohai Sea area, and its geological significance

Tianjin Branch, Bohai Oilfield Research Institute, CNOOC China Limited, Tianjin 300452, China

Received Date: 21 July 2016

Revised Date: 27 May 2017

Publish Date: 25 July 2017

Abstract

Abstract

For the purpose of better understanding of the formation, evolution and tectonic environment of the first unmetamorphosed granite oil pool in Bohai Sea area, the authors carried out a study of granite buried hill of Miaoxibei uplift. Based on petrography, LA-ICP-MS zircon U-Pb ages and whole-rock major and trace elements, the authors investigated the petrogenesis, magma source and tectonic setting. LA-ICP-MS zircon U-Pb data of the granite yielded weighted age of 155.4±2.5Ma, the granite is of cale-alkaline suite with positive Eu anomaly, both samples have the characteristics of depletion of heavy rare earth elements and en-richment of light rare earth elements, and the granite is strongly enriched in large ion lithophile elements (LILEs, e.g., Pb, Sr) but depleted in high field strength elements (HFSEs, e.g. Th, Nb, Zr). It is thus held that the crust experienced shortening and thickening rapidly because of the pressure of Yangtze plate and the Jiamusi Mongolia block during the early Middle Jurassic, and that, due to the rising temperature, the lower crust was subjected to partial melting, which eventually surged and invaded, resulting in the formation of peraluminous S-type granite in the Miaoxibei uplift buried hill.
- Miaoxibei uplift /
- granite /
- buried hill /
- LA-ICP-MS zircon U-Pb dating /
- Yenshanian /
- geochemistry

FullText(HTML)

References

[1]	夏庆龙, 田立新, 周心怀, 等.渤海海域构造形成演化与变形机制[M].北京:石油工业出版社, 2012. Google Scholar
[2]	李德生.渤海湾含油气盆地的地质和构造特征[J].石油学报, 1980, 1(1): 6-20. doi: 10.7623/syxb198001002 CrossRef Google Scholar
[3]	朱夏, 陈焕疆, 孙兆才, 等.中国新生代构造与含油气盆地[J].地质学报, 1983, 3: 235-242. Google Scholar
[4]	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. Google Scholar
[5]	侯贵延, 钱祥麟, 宋新民.渤海湾盆地形成机制研究[J].北京大学学报(自然科学版), 1998, 34(4): 503-509. Google Scholar
[6]	万天丰.中国东部中、新生代板内变形构造应力场及其应用[M].北京:地质出版社, 1993. Google Scholar
[7]	宗国洪, 施央申, 王秉海.济阳盆地中生代构造特征及油气[J].地质论评, 1998, 44(3): 289-294. Google Scholar
[8]	赵越, 徐守礼.沿大型走滑断裂系的隆升[J].地质科学, 1996, 31 (1): 1-14. Google Scholar
[9]	Maruyama S, Seno T. Orogeny and relative plate motions: Example of the Japanese island[J]. Tectonophysics, 1986, 2:305-329. Google Scholar
[10]	漆家福, 张一伟, 陆克政, 等.渤海湾新生代断裂盆地的伸展模式及其动力学过程[J].石油实验地质, 1995, 17(4): 316-323. doi: 10.11781/sysydz199504316 CrossRef Google Scholar
[11]	张云慧, 刘福平, 金芳红.沙垒田、庙西凸起前第三纪地层研究[J].中国海上油气, 2001, 15(6): 381-387. Google Scholar
[12]	官大勇, 王应斌, 王永利, 等.渤海海域PL花岗岩潜山油藏储集层特征[J].大庆石油地质与开发, 2012, 31(2): 48-51. Google Scholar
[13]	王昕, 周心怀, 徐国盛, 等.渤海海域蓬莱9-1花岗岩潜山大型油气田储层发育特征与主控因素[J].石油与天然气地质, 2015, 36 (2): 262-270. doi: 10.11743/ogg20150211 CrossRef Google Scholar
[14]	李建平, 周心怀, 王国芝.蓬莱9-1潜山岩性组成及其对储层发育的控制[J].地球科学(中国地质大学学报), 2014, 39(10): 1421-1430. Google Scholar
[15]	宗奕, 梁建设, 刘丽芳.庙西凹陷构造特征[J].岩性油气藏, 2012, 24(1): 36-39, 79. Google Scholar
[16]	Van Achterbergh E, Ryan C, Jackson S, et al. Appendix 3 data reduction software for LA-ICP-MS in"Laser-Ablation-ICPMS in the Earth Sciences" [J]. Mineralogical Association of Canada Short Course, 2001, 29:239-243. Google Scholar
[17]	Ludwig K R. ISOPLOT 3.00: A Geochronological toolkit for Microsoft Excel[M]. Berkeley Geochronological center special publication, Berkeley, 2003. Google Scholar
[18]	Hoskin P W O, Schaltegger U. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1): 27-62. doi: 10.2113/0530027 CrossRef Google Scholar
[19]	Peccerillo A, Taylor A R. Geochemistry of Eocene calc-alkaline volcanic rocks from the kastamou area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58: 63-81. doi: 10.1007/BF00384745 CrossRef Google Scholar
[20]	Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Socity, Landon, Special Publications, 1989, 42(1): 313-345. doi: 10.1144/GSL.SP.1989.042.01.19 CrossRef Google Scholar
[21]	宋彪, 乔秀夫.辽北辉绿岩墙(床)群及二道沟组玄武岩锆石年龄及其构造意义[J].地学前缘(中国地质大学(北京), 北京大学), 2008, 15(3): 250-262. Google Scholar
[22]	Ge X Y, Li X H, Chen Z G, et a1. Geochemistry and petrogenesis of Jurassic high Sr/low Y granitoids in eastern China: Constraints on crustal thickness[J]. Chinese Science Bulletin, 2002, 47: 961-968. Google Scholar
[23]	刘红涛, 孙世华, 刘建明, 等.华北克拉通北缘中生代高锶花岗岩类:地球化学与源区性质[J].岩石学报, 2002, 18(3): 257-274. Google Scholar
[24]	Ma C, Li Z, Ehlers C, et al. A post-collisional magmatic plumbing system: Mesozoic granitoid plutons from the Dabieshan high pressureand ultrahigh pressure metamorphic zone, east central China[J]. Lithos, 1998, 45: 431-456. doi: 10.1016/S0024-4937(98)00043-7 CrossRef Google Scholar
[25]	张旗, 王焰, 钱青, 等.中国东部燕山期埃达克岩的特征及其构造-成矿意义[J].岩石学报, 2001, 17(2): 236-244. Google Scholar
[26]	Zhang H F, Zheng J P. Geochemical characteristics and petrogenesis of Mesozoic basalts from the North China Craton: a case study in Fuxin, Liaoning Province[J]. Chinese Science Bulletin, 2003, 48: 924-930. doi: 10.1360/02wd0459 CrossRef Google Scholar
[27]	Qi J F, Li X G, Yu F S, et al. Cenozoic structural deformation and expression of the"Tan-Lu Fault Zone"in the West Sag of Liaohe Depression, Bohaiwan basin province[J]. China Earth Sciences, 2013, 56: 1707-1721. doi: 10.1007/s11430-013-4617-2 CrossRef Google Scholar
[28]	杜韫华, 代贤忠, 刘继昌.鲁北新生代隐伏火山岩及其石油地质意义[J].岩石学报, 1990, 3: 43-52. doi: 10.3321/j.issn:1000-0569.1990.03.005 CrossRef Google Scholar
[29]	赫英, 王定一, 廖永胜.胜利油田火山岩类、盆地演化及其CO₂-Au成藏成矿效应[J].地质科学, 36(4): 454-464. Google Scholar
[30]	于建国, 韩文功, 王金铎.中国东部断陷盆地中—新生代构造演化——以济阳凹陷为例[M].北京:石油工业出版社, 2009. Google Scholar
[31]	李小伟, 莫宣学, 赵志丹, 等.关于A型花岗岩判别过程中若干问题的讨论[J].地质通报, 2010, 29(Z1): 279-285. Google Scholar
[32]	Chappell B W. Aluminium saturation in I and S type granites and the characterization of fractionated hapogranites[J]. Lithos, 1999, 46: 535-551. doi: 10.1016/S0024-4937(98)00086-3 CrossRef Google Scholar
[33]	Clemens J D. S-Type granitic magmas-petrogenetic issues: Models and evidence[J]. Earth Science Reviews, 2003, 61: 1-18. doi: 10.1016/S0012-8252(02)00107-1 CrossRef Google Scholar
[34]	Liegeois J P, Black R. Alkaline magmatism subsequent to collision in the Pan-African belt of the Adrar des Iforas (Mali)[J]. Geological Society, London, Special Publications, 1987, 30: 381-401. doi: 10.1144/GSL.SP.1987.030.01.18 CrossRef Google Scholar
[35]	Wolf M B, Landon D. Apitite dissolution into peraluminous haplogranitic melts: an experimental study of solubilities and mechanism[J]. Geochimica et Cosmochim Acta, 1994, 58: 4127-4115. doi: 10.1016/0016-7037(94)90269-0 CrossRef Google Scholar
[36]	Föster H J, Tischendorf G, Trumbull R B. An evaluation of the Rb VS (Y+Nb) discrimination diagram to infer tectonic setting of silicic igneous rock[J]. Lithos, 1997, 40: 261-293. doi: 10.1016/S0024-4937(97)00032-7 CrossRef Google Scholar
[37]	Batchelor R A, Bowden P. Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters[J]. Chemical Geology, 1985, 48: 43-55. doi: 10.1016/0009-2541(85)90034-8 CrossRef Google Scholar
[38]	吴福元, 孙德有.中国东部中生代岩浆作用与岩石圈减薄[J].长春科技大学学报, 1999, 29(4): 313-318. Google Scholar
[39]	赵海玲, 邓晋福, 贺怀宇, 等.造山带陆壳增厚的一个岩石学记录:以济南辉长岩及其包体研究为例[J].地学前缘, 1998, 5(4): 251-256. Google Scholar
[40]	李承东, 张旗, 苗来成.冀北中生代高Sr低Y和低Sr低Y型花地球化学、成因及其与成矿作用的关系[J].岩石学报, 2004, 20(2): 269-284. Google Scholar
[41]	李伍平, 李献华, 路风香.辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义[J].岩石学报, 2001, 17(2): 523-532. Google Scholar
[42]	王焰, 张旗.八达岭花岗杂岩的组成、地球化学特征及其意义[J].岩石学报, 2001, 17(4): 533-540. Google Scholar
[43]	王强, 赵振华, 许继锋, 等.扬子地块东部燕山期埃达克质(adakite-like)岩与成矿[J].中国科学(D辑), 2002, 32(S2): 127-136. Google Scholar
[44]	Defant M J, Drummond M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J]. Nature, 1990, 347: 662-665. doi: 10.1038/347662a0 CrossRef Google Scholar
[45]	Petford N, Atherton M P. Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith. Peru[J]. Journal of Petrology, 1996, 37: 1491-1521. doi: 10.1093/petrology/37.6.1491 CrossRef Google Scholar