渤海东部旅大29-1构造沙二段砂砾岩锆石定年及物源示踪
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摘要
为示踪辽东凹陷LD29-1构造沙二段(Es_2)砂岩沉积,对LD29-1-1、LD29-1-1Sa及LD29-1-2等3口井的沙二段砂岩6个岩屑样品进行了碎屑锆石U-Pb定年和锆石阴极发光(CL)图像分析。结果表明:LD29-1-1井样品中白垩纪(K)锆石含量高达41.2%,具有108 Ma峰值年龄,锆石柱状晶形完整,并且棱角明显;而LD29-1-1Sa及LD29-1-2井样品的中元古代(Pt_2)锆石含量高达74%～75%,中生代(Mz)锆石含量少,具有～1.5 Ga和～1.8 Ga双峰值特征,锆石晶体明显小于LD29-1-1井沉积物,并且晶形不完整、边缘均被磨圆。因此,认为LD29-1-1井沙二段砂岩为近源沉积,母岩为长兴岛凸起斜坡带中生界碎屑岩,而LD29-1-1Sa及LD29-1-2井沙二段砂体为远源沉积,母岩以辽东半岛西部复州地区广泛分布的中、上元古界沉积岩为主,在搬运至斜坡带时才混入少量中生界碎屑岩。
To trace the sedimentary source-to-sink systems of the Lvda 29-1 structure in the eastern Bohai Sea,six sandstone cuttings of the second Member of Shahejie Formation( Es_2) were collected from LD29-1-1,LD29-1-1Sa and LD29-1-2 for detrital zircon U-Pb dating and cathodoluminescence( CL) image analysis. The results showed that the sandstones of LD29-1-1 contained 41.2% Cretaceous( K) zircons and featured a 108 Ma peak,and the columnar crystals were characterized by sharp edges. The LD29-1-1Sa and LD29-1-2 sandstones contained 74%-75% Mesoproterozoic( Pt2) zircons with peaks at ～1.5 Ga and ～1.8 Ga,and the broken crystals were well rounded. We concluded that the Es_2 sandstones of LD29-1-1 were near-source deposited,and the provenance was the Mesozoic sedimentary rocks along the slope of the Changxingdao Uplift; the Es_2 sandstones of LD29-1-1Sa and LD29-1-2 were distal from the source area and were dominated by the widespread Mesoproterozoic and Neoproterozoic sedimentary rocks exposed in Fuzhou on the western Liaodong Peninsula,with only a slight influence of Mesozoic sedimentary rocks from the slope of the Changxingdao Uplift.
To trace the sedimentary source-to-sink systems of the Lvda 29-1 structure in the eastern Bohai Sea,six sandstone cuttings of the second Member of Shahejie Formation( Es_2) were collected from LD29-1-1,LD29-1-1Sa and LD29-1-2 for detrital zircon U-Pb dating and cathodoluminescence( CL) image analysis. The results showed that the sandstones of LD29-1-1 contained 41.2% Cretaceous( K) zircons and featured a 108 Ma peak,and the columnar crystals were characterized by sharp edges. The LD29-1-1Sa and LD29-1-2 sandstones contained 74%-75% Mesoproterozoic( Pt2) zircons with peaks at ～1.5 Ga and ～1.8 Ga,and the broken crystals were well rounded. We concluded that the Es_2 sandstones of LD29-1-1 were near-source deposited,and the provenance was the Mesozoic sedimentary rocks along the slope of the Changxingdao Uplift; the Es_2 sandstones of LD29-1-1Sa and LD29-1-2 were distal from the source area and were dominated by the widespread Mesoproterozoic and Neoproterozoic sedimentary rocks exposed in Fuzhou on the western Liaodong Peninsula,with only a slight influence of Mesozoic sedimentary rocks from the slope of the Changxingdao Uplift.
引文
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[12]朱红涛,徐长贵,朱筱敏,等.陆相盆地源—汇系统要素耦合研究进展[J].地球科学,2017,42(11):1851-1870.[Zhu Hongtao,Xu Changgui,Zhu Xiaomin,et al. Advances of the source-tosink units and coupling model research in continental basin[J].Earth Science,2017,42(11):1851-1870.]
[13]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,2017,42(11):1984-1993.[Zhao Meng,Xu Changgui,Du Xiaofeng,et al. Detrital zircon UPb geochronology and provenance tracing of the fan deltas along the southwestern slope of the Shijiutuo uplift[J]. Earth Science,2017,42(11):1984-1993.]
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[18] Cawood P A,Hawkesworth C J,Dhuime B. Detrital zircon record and tectonic setting[J].Geology,2012,40(10):875-878.
[19] Shao L,Cao L C,Qiao P J,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.
[20]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.]
[21]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.]
[22]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.]
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[24] Sircombe K N,Hazelton M L. Comparison of detrital zircon age distributions by kernel functional estimation[J]. Sedimentary Geology,2004,171(1/2/3/4):91-111.
[25] Vermeesch P. Statistical uncertainty associated with histograms in the earth sciences[J].Journal of Geophysical Research,2005,110(B2):B02211.
[26] Vermeesch P. On the visualisation of detrital age distributions[J].Chemical Geology,2012,312-313:190-194.
[27] Yang J H,Wu F Y,Zhang Y B,et al. Identification of mesoproterozoic zircons in a Triassic dolerite from the Liaodong Peninsula,Northeast China[J]. Chinese Science Bulletin,2004,49(18):1958-1962.
[28] Luo Y,Sun M,Zhao G C,et al. A comparison of U–Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe Groups:constraints on the evolution of the Jiao-Liao-Ji Belt,North China Craton[J]. Precambrian Research,2008,163(3/4):279-306.
[29] Yang D B,Xu W L,Xu Y G,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,2012,216-219:162-176.
[30] Meng E,Liu F L,Cui Y,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.]
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