大青山地区侏罗纪陆相沉积盆地形成、迁移及演化规律

恢复了大青山地区侏罗纪盆地的原形，并对盆地的迁移，演化规律和阶段进行了详细研究，提出石拐－老道沟株罗纪盆地是早侏罗世晚期在古生代地层岩片与北部变质岩岩片之间发育起来的东西向延展的带状盆地。古地形表现北高南低，西高东低；中侏罗世盆地范围达最大，中株罗世末期的一次燕山构造运动，使盆地的性质发生了明显的改变，由早，中株罗世的弱拉伸构造环境转变为晚侏罗世的挤压构造环境，古气候由温暖潮湿气候变为干旱气候，晚侏罗世末期，随着大规模的逆冲推覆构造的发育而结束盆地的演化历史。

The Formation, Moving and Evolution Pattern of Jurassic Terrestrial Deposit Basin in Daqingshan Region

The authors have reconstructed the original shape of Jurassic basin in Daqing-shan region and discussed the moving and evolution pattern of the basin. The basin developed between Paleozic strata sliver and metamorphic rock sliver in late stage of early Jurassic and ex-tended in latitude direction. The paleo - terrene of the basin is higher in north and west than in south and east. The boundary of basin is largest in Changhangou stage of middle Jurassic. After middle Jurassic, the region took place Yanshan movement, and then the basin characteristic were changed obviously from weakly extending environment of early and middle Jurassic to ex-truding environment of late Jurassic, and the paleo - climate of the basin changed from warmth and wetness to dry. The basin finished the evolution history in the late stage of late Jurassic with the development of thrust.