松辽盆地南部中生代火山岩: 锆石U-Pb年代学及其对基底性质的制约

裴福萍; 许文良; 杨德彬; 纪伟强; 于洋; 张兴洲

松辽盆地南部中生代火山岩: 锆石U-Pb年代学及其对基底性质的制约

吉林大学地球科学学院, 吉林长春 130061

基金项目:

国家自然科学基金项目 40672038

国家自然科学基金项目 40739905

详细信息

作者简介:
裴福萍(1969-), 女, 博士研究生, 主要从事岩浆作用地球动力学研究.E-mail: peifp@jlu.edu.cn

通讯作者:
许文良(1959-), E-mail: xuwl@jlu.edu.cn, Tel: +86-431-88502080

中图分类号: P511
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- 被引次数: 0
出版历程
- 收稿日期: 2008-01-28
- 刊出日期: 2008-09-25

Mesozoic Volcanic Rocks in the Southern Songliao Basin: Zircon U-Pb Ages and Their Constraints on the Nature of Basin Basement

College of Earth Sciences, Jilin University, Changchun 130061, China

摘要

摘要: 为了确定松辽盆地南部中生代火山岩的形成时代, 本文对位于盆地南部7个钻遇中生代火山岩的岩芯样品进行了锆石LA~ICP-MSU-Pb定年.松辽盆地南部中生代含火山岩地层主要包括火石岭组和营城组, 其中火石岭组火山岩由玄武安山岩-粗安岩-粗面英安岩组成, 营城组火山岩由玄武质粗面安山岩-粗面安山岩-流纹岩组成.锆石阴极发光(CL)图像和Th/U比值显示, 所测锆石均具有岩浆成因的特点, 锆石的LA-ICP-MSU-Pb定年结果表明, 松辽盆地南部中生代火山岩形成时代介于110b133Ma, 其中火石岭组火山岩形成于129-133Ma, 即早白垩世早期, 营城组火山岩形成于110~119/Via, 即早白垩世晚期.捕获锆石的定年结果显示, 本区基底中存在中晚侏罗世(155~169Ma)、印支期(218~236Ma)、海西期(254/Via、294Ma)、加里东期(413Ma)和前寒武纪(1823/Via和2542Ma)岩浆事件, 这与基底岩石中锆石U—Pb的定年结果相吻合.
- 松辽盆地 /
- 中生代火山岩 /
- 锆石U-PB年龄 /
- 基底
Abstract: LA-ICP-MS zircon U-Pb dating results are reported for the Mesozoic volcanic rocks from seven wells in the southern Songliao basin in order to constraint their formation time. The Mesozoic volcanic rocks are mainly located in Huoshiling Formation and Yingcheng Formation. The former consists of basaltic andesite, trachyandesite and dacite, the latter is composed of basaltic trachyandesite, trachyandesite and rhyolite. The cathodoluminesence (CL) images and high Th/U ratios of the zircons suggest their magmatic origin. LA-ICP-MS zircon U-Pb dating results indicate that the Mesozoic volcanic rocks in the southern Songliao Basin formed between 110 Ma and 133 Ma. The volcanic rocks in the Huoshiling Formation were erupted during 129-133 Ma, namely early period of the Early Cretaceous, while those in the Yingcheng Formation formed between 110 Ma and 119 Ma, namely late period of the Early Cretaceous. The dating results of captured zircons show that the Middle-Late Jurassic (155-169 Ma), Indosinian (218-236 Ma), Hercynian (254 Ma, 294 Ma), Caledonian (413 Ma), and Precambrian (1 823 Ma and 2 542 Ma) magmatic events had taken place in the basin basement, which is consistent with the zircon U-Pb dating results from the basin basement rocks.
- Songliao basin /
- Mesozoic volcanic rocks /
- zircon U-Pb age /
- basement

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图 1 松辽盆地南部构造略图

F1. 贺根山-嫩江断裂; F2. 牡丹江断裂; F3. 佳木斯-依兰断裂; F4. 敦化-密山断裂

Fig. 1. Sketch map showing the tectonic of the southern Songliao basin

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图 2 部分钻井岩性柱状图和采样位置

Fig. 2. Columns of some wells showing lithology and sampling location

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图 3 松辽盆地南部中生代火山岩中锆石CL图像

Fig. 3. CL images of selected zircons from the Mesozoic volcanic rocks in the southern Songliao basin

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图 4 松辽盆地中生代火山岩U-Pb谐和图(a~g)及年龄数据统计(h)

Fig. 4. Concordia plots of zircons from the Mesozoic volcanic rocks in the southern Songliao basin (a-g) and age cumulative diagram (h)

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表 1 松辽盆地南部中生代火山岩岩芯样品的地质及岩相学特征

Table 1. Geological and petrographic characteristics of the Mesozoic volcanic rocks in the southern Songliao basin

表 2 松辽盆地南部中生代火山岩中锆石LA-ICP-MS U-Pb分析结果

Table 2. LA-ICP-MS zircon U-Pb dating data from the Mesozoic volcanic rocks in the southern Songliao basin

表 3 样品SN72-5 K-Ar测年结果

Table 3. Sample SN 72-5 K-Ar dataing age

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