| 辽西中生代波罗赤盆地特征及盆地性质探讨 |
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| 引用本文： | 鲍庆忠,张立东,郭胜哲,董万德.辽西中生代波罗赤盆地特征及盆地性质探讨[J].地质与资源,2002,11(1):1-8. |
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| 作者姓名： | 鲍庆忠 张立东 郭胜哲 董万德 |
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| 作者单位： | 1. 东北大学 资源与土木工程学院, 辽宁 沈阳 110004;2. 沈阳地质矿产研究所, 辽宁 沈阳 110033;3. 辽宁地质勘查院, 辽宁 大连 116100 |
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| 基金项目： | 中国地质调查局“K50E015024(朱碌科镇幅)、K50E016024(波罗赤幅)两幅1:5万区域地质调查”项目部分研究成果. |
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| 摘 要： | 本文是朱碌科镇幅等两幅1：5万区调成果的一部分，通过分析盆地内的物质记录、火山岩特征、控盆构造，说明辽西地区中生代陆相沉积盆地的形成具有明显的旋回性，每一旋回均以强烈的火山喷发为先导，继而盆地沉降接受沉积.从早期到晚期，波罗赤盆地从西向东迁移.盆地早期形成于压性环境，晚期形成于拉张环境.波罗赤盆地形成时代为中侏罗世—晚白垩世早期.
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| 关 键 词： | 波罗赤盆地 物质记录 控盆构造 盆地性质 |
| 文章编号： | 1671-1947(2002)01-0001-08 |
| 收稿时间： | 2001-12-11 |
| 修稿时间： | 2001年12月11 |
GEOLOGICAL CHARACTERISTICS AND NATURES OF MESOZOIC CONTINENTAL BASIN IN WESTERN LIAONING,CHINA |
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| BAO Qing-zhong ,ZHANG Li-dong ,GUO Sheng-zhe ,Dong Wan-de.GEOLOGICAL CHARACTERISTICS AND NATURES OF MESOZOIC CONTINENTAL BASIN IN WESTERN LIAONING,CHINA[J].Geology and Resources,2002,11(1):1-8. |
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| Authors: | BAO Qing-zhong ZHANG Li-dong GUO Sheng-zhe Dong Wan-de |
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| Institution: | 1. Institute of Resources and Civil Engineering, Northeast University, Shenyang 110004, China;2. Shenyang Institute of Geology and Mineral Recourses, Shenyang 110033, China;3. Liaoning Instiute of Geologic Exploration, Dalian 116100, China |
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| Abstract: | Based on the 1:50000regional geolo gical survey in Zhuluke-Boluochi sh eet,the basin-controlling structu re,sedimentary substances and volcani c rocks in Boluochi Basin are studied.By analyzing the volcanic materials,ter-rigenous clastic sediments and their sequence,the formation of Boluoch i Basin may be divided into three cycles.In each cycle,the sedimentary process begins with volcanic explosion,followe d by continental clastic deposition.The polycyclic formation of the basin is quite clear.The basin is in compression stress e nvironment in Middle Jurassic,and e xtension in Late Jurassic to Early Cretaceous.S imultaneously,the center of the Mesozoic basin transferred from the West(Zhongsanjia-Maozhengou)to East(Maozhengou-Huangdaoyingzi). |
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| Keywords: | Boluochi Mesozoic continental basin material record polycyclicity compresion stress environment ex-tension stress environment |
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