[an error occurred while processing this directive] 世界地质 2019, 38(4) 1032-1043 DOI:   10.3969/j.issn.1004-5589.2019.04.014  ISSN: 1004-5589 CN: 22-1111/P
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松辽盆地
松科2井
登娄库组
沉积序列
本文作者相关文章
刘硕
高有峰
尹永康
刘海波
李宏浩
王璞臖
PubMed
Article by Liu S
Article by Gao Y
Article by Yin Y
Article by Liu H
Article by Li H
Article by Wang P
松辽盆地大陆科学钻探“松科2井”登娄库组二段沉积序列精细刻画及时代归属
刘硕1,2, 高有峰1,3, 尹永康2, 刘海波2, 李宏浩2, 王璞臖1,2
1. 吉林大学 东北亚生物演化与环境教育部重点实验室, 长春 130026;
2. 吉林大学 地球科学学院, 长春 130061;
3. 吉林大学 古生物学与地层学研究中心, 长春 130026
摘要： 松辽盆地大陆科学钻探"松科2井"连续获取登娄库组二段岩芯105.05 m，岩芯收获率为99.1%，是迄今获取的最连续完整的沉积记录。笔者对该段岩芯进行了厘米级沉积地质描述（分层厚度2~5 cm），揭示其岩性-岩相沉积序列。登娄库组二段共识别9种岩石类型，为辫状河相的废弃河道和河道亚相，并且进一步划分为河道淤积、沙滩、心滩3种沉积微相。碎屑锆石LA-ICP-MS U-Pb测年结果中登娄库组二段最年轻碎屑锆石年龄为102±4 Ma，表明松辽盆地徐家围子断陷该时期已经进入阿尔必晚期。
关键词： 松辽盆地   松科2井   登娄库组   沉积序列  
Fine description and geological age delineation of sedimentary sequences of the second member of Denglouku Formation based on ICDP scientific drilling borehole in Songliao Basin (SK2)
LIU Shuo1,2, GAO You-feng1,3, YIN Yong-kang2, LIU Hai-bo2, LI Hong-hao2, WANG Pu-jun1,2
1. Key Laboratory for Evolution of Past Life and Environment in Northeast Asia(Jilin University), Ministry of Education, Changchun 130026, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, China;
3. Research Center of Paleontology and Stratigraphy, Jilin University, Changchun 130026, China
Abstract: International Continental Scientific Drilling Project (ICDP) in the Songliao Basin, named SK2, has obtained 105.05 m of continuous core of the second member of Denglouku Formation, with core recovery of 99.1%, which is the most continuous and complete sedimentary record of this member. The authors carry out cen-timeter-scale core description (2~5 centimeter per layer) to reveal the lithology, lithofacies and sedimentary se-quences. Nine rock types have been identified in the second member of Denglouku Formation, including abandoned channel and channel sub-facies of braided river facies, which are further divided into three kinds of sedimentary mi-crofacies, i. e., channel siltation, sand bar and mid-channel bar. The youngest age of detrital zircon LA-ICP-MS U-Pb isotopic dating results of the second member of Denglouku Formation is 102±4 Ma, indicating that the sec-ond member of Denglouku Formation formed in Xujiaweizi fault depression of Songliao Basin belongs to the late Al-bian period.
Keywords: Songliao Basin   SK2   Denglouku Formation   sedimentary sequence  
收稿日期 2019-07-17 修回日期 2019-09-21 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2019.04.014
基金项目:

国家重点研发计划项目（2019YFC0605402）、国家自然科学基金（41790453）与中国地质调查局油气基础性公益性地质调查项目（DD20189702）联合资助。

通讯作者: 高有峰(1982),男,博士,副教授,主要从事沉积学与地层学研究。E-mail:gaoyoufeng@jlu.edu.cn
作者简介:
作者Email: gaoyoufeng@jlu.edu.cn
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