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《Journal of Stratigraphy》 2008-01
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SHRIMP ZIRCON U-Pb GEOCHRONOLOGY OF VOLCANIC ROCKS AND DISCUSSION ON THE GEOLOGICAL TIME OF THE YINGCHENG FORMATION OF THE NORTHERN SONGLIAO BASIN

ZHANG Feng-qi1), CHEN Han-lin1), DONG Chuan-wan1),PANG Yan-ming2), SHU Ping2), WANG Yan-lou1) and YANG Shu-feng1)1) Earth Science Department of Zhejiang University, Hangzhou 310027;2) Exploration and Development Research Institute of Daqing Oilfield, Daqing 163712  
The age of the Yingcheng Formation in the Songliao Basin has been disputed. A suite of volcanic intermediate rocks to acidites, mainly acidic eruptive rocks, occurs widely in the Yingcheng Formation in the Xujiaweizi fault-depression in the northern Songliao Basin. SHRIMP zircon U-Pb geochronology gives ages between 111Ma and 113Ma for the volcanic rocks indicating that the volcanic succession formed around Aptian-Albian of the Early Cretaceous. Accordingly it is concluded that this suite of volcanic rocks was emplaced at the middle-upper part of the Yingcheng Formation. Based on available information, the age of the Yingcheng Formation in the northern Songliao Basin is most likely between Hauterivian and Albian.
【Fund】: 大庆油田勘探开发研究院天然气开发项目
【CateGory Index】: P534.53
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