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[1]赵 梦 杜晓峰 王清斌 赵 婧 郝轶伟.渤海东部蓬莱15-2构造东营组、馆陶组砂岩碎屑锆石定年及物源示踪[J].中国海上油气,2019,31(04):46-54.[doi:10.11935/j.issn.1673-1506.2019.04.006]
 ZHAO Meng DU Xiaofeng WANG Qingbin ZHAO Jing HAO Yiwei.Detrital zircon dating and provenance implication of sandstone in Dongying and Guantao Formations of Penglai 15-2 structure in eastern Bohai sea[J].China Offshore Oil and Gas,2019,31(04):46-54.[doi:10.11935/j.issn.1673-1506.2019.04.006]
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渤海东部蓬莱15-2构造东营组、馆陶组砂岩碎屑锆石定年及物源示踪()

《中国海上油气》[ISSN:1673-1506/CN:11-5339/TE]

卷:
第31卷
期数:
2019年04期
页码:
46-54
栏目:
油气勘探
出版日期:
2019-07-25

文章信息/Info

Title:
Detrital zircon dating and provenance implication of sandstone in Dongying and Guantao Formations of Penglai 15-2 structure in eastern Bohai sea
文章编号:
1673-1506(2019)04-0046-09
作者:
赵 梦 杜晓峰 王清斌 赵 婧 郝轶伟
(中海石油(中国)有限公司天津分公司 天津 300459)
Author(s):
ZHAO Meng DU Xiaofeng WANG Qingbin ZHAO Jing HAO Yiwei
(CNOOC China Limited, Tianjin Branch, Tianjin 300459, China)
关键词:
蓬莱15-2构造 东营组 馆陶组 碎屑锆石定年 物源示踪
Keywords:
Penglai 15-2 structure Dongying Formation Guantao Formation detrital zircon dating provenance implication
分类号:
TE121.3
DOI:
10.11935/j.issn.1673-1506.2019.04.006
文献标志码:
A
摘要:
为了示踪渤海东部蓬莱15-2构造东营组(Ed2)、馆陶组(N1g)砂岩沉积,对PL15-2-7及PL15-2-12d井的4个岩屑样品进行了碎屑锆石U-Pb定年分析,发现PL15-2-7井东营组二段(Ed2)砂岩仅含有太古代(Ar)—古元古代(Pt1)碎屑锆石,具有突出的1 863 Ma峰值,不含中生代锆石,母岩为庙西北凸起南部古元古代变质岩,不受凸起鞍部的侏罗纪花岗岩影响; 而PL15-2-12d井馆陶组(N1g)砂岩样品的侏罗纪(J)锆石含量高达39.2%,并具有突出的159 Ma峰值,母岩为庙西北凸起鞍部的侏罗纪花岗岩,但该井还受到盆外水系影响,沉积物富含古元古代(Pt1)和中元古代(Pt2)锆石,并具有独特的1 486 Ma峰值。通过与辽东半岛及山东长岛地区的中、上元古界地层对比,认为PL15-2-12d井馆陶组(N1g)砂岩的盆外物源为旅顺地区的上元古界沉积岩,经老铁山水系搬运至研究区再沉积,不受以约1 600 Ma峰值为特征的辽宁复州、大连及山东长岛地区的上元古界影响。
Abstract:
In order to trace the sandstone deposits of Dongying Formation(Ed2)and Guantao Formation(N1g)in Penglai 15-2 structure in the eastern Bohai sea, detrital zircon U-Pb dating analysis of four cutting samples from Well PL15-2-7 and PL15-2-12d was carried out. It was found that the sandstone of the Second Member of Dongying Formation(Ed2)in Well PL15-2-7 contains only Archean(Ar)-Paleoproterozoic(Pt1)detrital zircon, with a prominent peak value of 1 863 Ma and no Mesozoic zircon. The parent rock was Paleoproterozoic metamorphic rock in the south of Miaoxibei uplift, which was not affected by Jurassic granite in the saddle part of the uplift; while the Jurassic(J)zircon content of the sandstone samples of the Guantao Formation(N1g)in Well PL15-2-12d was up to 39.2%, with a prominent peak value of 159 Ma. The parent rock was Jurassic granite in the saddle part of Miaoxibei uplift, but the well was also influenced by an extrabasinal source, and the sediments were rich in Paleoproterozoic(Pt1)and Mesoproterozoic(Pt2)zircons, with a unique peak value of 1 486 Ma. Compared with the Mesoproterozoic and Neoproterozoic strata in the Liaodong Peninsula and Changdao area of Shandong Province, it was considered that the extrabasinal source rocks of the Guantao Formation(N1g)in the Well PL15-2-12d were the Neoproterozoic sedimentary rocks in the Lyushun area, which were transported to the studied area by the Laotie mountain water system and then deposited, and were not affected by the Neoproterozoic in the Fuzhou, Dalian areas of Liaoning Province and Changdao areas of Shandong Province characterized by the peak value of about 1 600 Ma.

参考文献/References:

[1] CAWOOD P A,HAWKESWORTH C J,DHUIME B.Detrital zircon record and tectonic setting[J].Geology,2012,40(10):875-878. [2] CAWOOD P A,NEMCHIN A A,FREEMAN M,et al.Linking source and sedimentary basin:Detrital zircon record of sediment flux along a modern river system and implications for provenance studies[J].Earth and Planetary Science Letters,2003,210(1/2):259-268. [3] DEGRAAFF-SURPLESS K,GRAHAM S A,WOODEN J L,et al.Detrital zircon provenance analysis of the Great Valley Group,California:Evolution of an Arc-Forearc System[J].Geological Society of America Bulletin,2002,114(12):1564-1580. [4] LOWE D,SYLVESTER P,ENACHESCU M.Provenance and paleodainage patterns of Upper Jurassic and Lower Cretaceous synrift sandstones in the Flemish Pass Basin,offshore Newfoundland,East Coast of Canada[J].AAPG Bulletin,2011,95(8):1295-1320. [5] MOECHER D P,SAMSON S D.Differential zircon fertility of source terranes and natural bias in the detrital zircon record:Implications for sedimentary provenance analysis[J].Earth and Planetary Science Letters,2006,247(3):252-266. [6] SHAO Lei,CAO Licheng,QIAO Peijun,et al.Cretaceous-Eocene provenance connections between the Palawan Continental Terrane and the Northern South China Sea Margin[J].Earth and Planetary Science Letters,2017,477:97-107. [7] DU Xiaofeng,XU Changgui,PANG Xiaojun,et al.Quantitative reconstruction of source-to-sink systems of the First and Second Members of the Shahejie Formation of the Eastern Shijiutuo Uplift,Bohai Bay Basin,China[J].Interpretation,2017,5(4):85-102. [8] 李欢,杨香华,朱红涛,等.渤中西环古近系东营组物源转换与沉积充填响应[J].沉积学报,2015,33(1):36-48. LI Huan,YANG Xianghua,ZHU Hongtao,et al.The provenance transformation and sedimentary filling response of Paleogene Dongying Formation in western slope of Bozhong Sag[J].Acta Sedimentologica Sinica,2015,33(1):36-48. [9] 刘强虎,朱筱敏,李顺利,等.沙垒田凸起前古近系基岩分布及源-汇过程[J].地球科学——中国地质大学学报,2016,41(11):1935-1949. LIU Qianghu,ZHU Xiaomin,LI Shunli,et al.Pre-Paleogene bedrock distribution and source-to-sink system analysis in the Shaleitian Uplift[J].Earth Science—Journal of China University of Geosciences,2016,41(11):1935-1949. [10] 赵梦,徐长贵,杜晓峰,等.石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪[J].地球科学——中国地质大学学报,2017,42(11):1984-1993. ZHAO Meng,XU Changgui,DU Xiaofeng,et al.Detrital zircon U-Pb geochronology and provenance tracing of the fan deltas along the southwestern slope of the Shijiutuo Uplift[J].Earth Science—Journal of China University of Geosciences,2017,42(11):1984-1993. [11] 周心怀,黄雷,王昕,等.渤海蓬莱9-1中生代花岗岩体岩石地球化学特征及其区域构造意义[J].岩石学报,2016,32(6):1839-1850. ZHOU Xinhuai,HUANG Lei,WANG Xin,et al.Geochemistry of Mesozoic granite from Penglai 9-1 oilfield of Bohai Sea and its regional tectonic significance[J].Acta Petrologica Sinica,2016,32(6):1839-1850. [12] 赵国祥,王清斌,杨波,等.渤海海域庙西北凸起中生代花岗岩LA-ICP-MS锆石U-Pb测年及其地质意义[J].地质通报,2017,36(7):1204-1217. ZHAO Guoxiang,WANG Qingbin,YANG Bo,et al.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. [13] 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):1521-1530. LI Jianping,ZHOU Xinhuai,WANG Guozhi.Lighologic Constitution and its control on reservoir development on Penglai 9-1 buried hill,Bohai Sea Basin[J].Earth Science—Journal of China University of Geosciences,2014,39(10):1521-1530. [14] 冯冲,王清斌,杨波,等.渤海海域蓬莱9-1构造潜山中生代花岗岩元素地球化学特征及其地质意义[J].地质学报,2016,90(4):752-768. FENG Chong,WANG Qingbin,YANG Bo,et al.Geochemical characteristic of Mesozoic granite of the Penglai 9-1 buried hill,Bohai Bay and its geological significance[J].Acta Geologica Sinica,2016,90(4):752-768. [15] 王明臣,官大勇,刘朋波,等.渤海蓬莱9-1油藏花岗岩储层特征与成储化条件分析[J].地质科技情报,2016,35(6):83-89. WANG Mingchen,GUAN Dayong,LIU Pengbo,et al.Characteristics and formation conditions of the Penglai 9-1 granite oil reservoir in Bohai Gulf Basin[J].Geological Sicence and Technology Information,2016,35(6):83-89. [16] 王昕,周心怀,徐国胜,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. WANG Xin,ZHOU Xinhuai,XU Guosheng,et al.Characteristics and controlling factors of reservoirs in Penglai9-1 large-scale oilfield in buried granite hills,Bohai Sea[J].Oil & Gas Geology,2015,36(2):262-270. [17] 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其石油地质意义[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. [18] 白冰,王清斌,赵国祥,等.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,et al.Cenozoic tectonic evolution of PL9-1 structure:An evidence of apatite fission track[J].Acta Petrolei Sinica,2015,36(9):1098-1107. [19] 官大勇,王昕,刘军钊,等.庙西北凸起不整合面结构及其与油气成藏关系[J].海洋石油,2013,33(1):29-32. GUAN Dayong,WANG Xin,LIU Junzhao,et al.The architecture of unconformity in the Miaoxibei uplift and its effect on hydrocarbon accumulation[J].Offshore Oil,2013,33(1):29-32. [20] 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(地质),2001,15(6):381-387. ZHANG Yunhui,LIU Fuping,JIN Fanghong.PreTertiary stratigraphy of Shaleitian and Miaoxi uplifts[J].China Offshore Oil and Gas(Geology),2001,15(6):381-387. [21] 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. [22] 刘朋波,王昕,官大勇,等.渤海东部庙北地区古近系层序与沉积特征[J].地质科技情报,2012,31(3):1-7. LIU Pengbo,WANG Xin,GUAN Dayong,et al.Sequence and sedimentary characteristics of Paleogene in Miaobei area,East Bohai Bay[J].Geological Science and Technology Information,2012,31(3):1-7. [23] 韩少甲,赵俊峰,刘池洋,等.渤海海域庙西凹陷古近纪沙三段沉积期原盆面貌恢复[J].地质论评,2014,60(2):339-347. HAN Shaojia,ZHAO Junfeng,LIU Chiyang,et al.Restoration of original sedimentary extent of Miaoxi Sag in Bohai Sea during the sedimentary period of the Third Member of Shahejie Formation in Paleogene[J].Geological Review,2014,60(2):339-347. [24] 姜培海.渤海湾地区古水系特征[J].中国海上油气(地质),1998,12(3):200-205. JIANG Peihai.Characteristics of paleo-current drainage in Bohai Bay Basin[J].China Offshore Oil and Gas(Geology),1998,12(3):200-205. [25] 鲜本忠,王震,马立驰,等.沉积区—剥蚀区古地貌一体化恢复及古水系研究:以渤海湾盆地辽东地区馆陶组为例[J].地球科学——中国地质大学学报,2017,42(11):1922-1935. XIAN Benzhong,WANG Zhen,MA Lichi,et al.Paleao-Drainage system and integrated Paleo-Geomorphology restoration in depositional and erosional areas:Guantao Formation in East Liaodong area,Bohai Bay Basin,China[J].Earth Science—Journal of China University of Geosciences,2017,42(11):1922-1935. [26] CAMPBELL I H,REINERS P W,ALLEN C M,et al.He-Pb double dating of detrital zircons from the Ganges and Indus rivers:Implication for quantifying sediment recycling and provenance studies[J].Earth and Planetary Science Letters,2005,237:402-432. [27] SIRCOMBE K N,HAZELTON M L.Comparison of detrital zircon age distributions by Kernel functional estimation[J].Sedimentary Geology,2004,171(1-4):91-111. [28] VERMEESCH P.On the visualization of detrital age distribution[J].Chemical Geology,2012,312-313:190-194. [29] VERMEESCH P.Statistical uncertainty associated with histograms in the earth sciences[J].Journal of Geophysical Research,2005,110,B02211. [30] MENG En,LIU Fulai,CUI Ying,et al.Zircon U-Pb and Lu-Hf isotopic and whole-rock geochemical constraints on the protolith and tectonic history of the Changhai metamorphic supracrustal sequence in the Jiao-Liao-Ji Belt,southeast Liaoning Province,northeast China[J].Precambrian Research,2013,233:297-315. [31] 高林志,张传恒,陈寿铭,等.辽东半岛细河群沉积岩碎屑锆石SHRIMP U-Pb年龄及其地质意义[J].地质通报,2010,29(8):1113-1122. GAO Linzhi,ZHANG Chuangheng,CHEN Shouming,et al.Detrital zircon SHRIMP U-Pb age from the Diaoyutai Formation,Xihe Group in Liaodong Peninsula,China and its geological significance[J].Geological Bulletin of China,2010,29(8):1113-1122. [32] YANG Debin,XU Wenliang,XU Yigang,et al.U-Pb ages and Hf isotope data from detrital zircons in the Neoproterozoic sandstones of northern Jiangsu and southern Liaoning Provinces,China:Implications for the Late Precambrian evolution of the southeastern North China Craton[J].Precambrian Research,2012,162-176. [33] 初航,陆松年,王惠初,等.山东长岛地区蓬莱群辅子夼组碎屑锆石年龄谱研究[J].岩石学报,2011,27(4):1017-1028. CHU Hang,LU Songnian,WANG Huichu,et al.U-Pb age specrum of detrital zircons from the Fuzikuang Formation,Penglai Group in Changdao,Shandong Province[J].Acta Petrologica Sinica,2011,27(4):1017-1028. [34] 中国地质调查局.1:100万中国地质图.全国地质资料馆,2013.http:∥geodata.ngac.cn/Map/Detail.aspx?MapId=EC7E1A7A7AD81954E0430100007F182E. [35] 辽宁省地质矿产局.辽宁省区域地质志[M].北京:地质出版社,1989:56-125. [36] 山东省地质矿产局.山东省区域地质志[M].北京:地质出版社,1991:6-78.

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备注/Memo

备注/Memo:
*“十三五”国家科技重大专项“渤海海域勘探新领域及关键技术研究(编号:2016ZX05024-003)”部分研究成果。 第一作者简介: 赵梦,女,博士,工程师,主要从事沉积学、地质学研究。地址:天津市滨海新区海川路2121号B座(邮编:300459)。E-mail:zhaomeng5@cnooc.com.cn。
更新日期/Last Update: 1900-01-01