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辽西中生代波罗赤盆地特征及盆地性质探讨
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
作者姓名:鲍庆忠  张立东  郭胜哲  董万德
作者单位:东北大学资源与土木工程学院,辽宁沈阳,110004;沈阳地质矿产研究所,辽宁沈阳,110033;沈阳地质矿产研究所,辽宁沈阳,110033;辽宁地质勘查院,辽宁大连,116100
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.
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.

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:2001-12-11

GEOLOGICAL CHARACTERISTICS AND NATURES OF MESOZOIC CONTINENTAL BASIN IN WESTERN LIAONING,CHINA
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
Authors:BAO Qing-zhong     ZHANG Li-dong     GUO Sheng-zhe   Dong Wan-de
Affiliation: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
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).
Keywords:Boluochi Mesozoic continental basin  material record  polycyclicity  compresion stress environment  ex-tension stress environment
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