古地理学报 ›› 2011, Vol. 13 ›› Issue (6): 615-626. doi: 10.7605/gdlxb.2011.06.003

• 古地震 • 上一篇    下一篇

山东诸城晚白垩世古地震事件与恐龙化石埋藏*

何碧竹1 乔秀夫1 田洪水2 陈树清3 张艳霞3   

  1. 1 大陆构造与动力学国家重点实验室,中国地质科学院地质研究所,北京 100037
    2 山东建筑大学土木工程学院,山东济南 250014
    3 山东诸城市恐龙文化研究中心,山东诸城 262200
  • 收稿日期:2011-08-15 修回日期:2011-09-08 出版日期:2011-12-01 发布日期:2011-12-01
  • 作者简介:何碧竹,女,1965年生,博士,研究员,主要从事盆地构造分析及油气勘探目标综合研究。E-mail:hebizhu@vip.sina.com。
  • 基金资助:
    中石化科技部项目(编号:P05036)及国土资源部行业基金项目(编号:201011034)联合资助

Palaeoearthquake event and dinosaur fossil burial of the Late Cretaceous in Zhucheng of Shandong Province

He Bizhu1, Qiao Xiufu1, Tian Hongshui2, Chen Shuqing3, Zhang Yanxia3   

  1. 1 State Key Laboratory of Continental Tectonics and Dynamics,Institute of Geology,
    Chinese Academy of Geological Sciences(Beijing),Beijing 100037
    2 School of Civil Engineering, Shandong Jianzhu University,Jinan 250014, Shandong
    3 Dinosaur Research Center,Zhucheng 262200,Shandong
  • Received:2011-08-15 Revised:2011-09-08 Online:2011-12-01 Published:2011-12-01
  • About author:He Bizhu,born in 1965,is a doctor and researcher.Her research interests include tectonic analyses of basin and hydrocarbon reservoir targets evaluation.E-mail:hebizhu@vip.sina.com.

摘要: 在山东诸城库沟、龙骨涧、西见屯集群恐龙化石埋藏层——上白垩统王氏群辛格庄组与红土崖组中,发现存在脆性、塑性及液化等多种类型的软沉积物变形构造,主要包括负载构造、球—枕构造、挤入构造(火焰构造)、液化卷曲变形、液化脉状构造、混插沉积构造及地震断裂等典型的粗碎屑沉积物形成的古地震记录。多层的软沉积物变形构造及未变形沉积层间互出现,反映晚白垩世诸城地区地震活动频繁,地震活动具有多期性、间歇性及活动能量强—弱转换的脉动性。泥石流、洪泛平原沉积层中埋藏了大规模、顺层分布的恐龙(鸭嘴龙)骨骼化石,其中砂砾岩物源主要来自盆地南缘下白垩统的莱阳组和青山组。多层的古地震软沉积物变形构造层之间夹持着恐龙化石埋藏层,可能与盆地南缘诱发泥石流、埋藏大规模恐龙骨骼的突发性、强能量地震事件有关。

关键词: 软沉积物变形构造, 古地震成因, 恐龙化石埋藏, 上白垩统, 山东诸城

Abstract: Various and complex styles of soft-sediment deformation structures were recognized in the Upper Cretaceous of the Kugou-Longgujian-Xijiantun district at southwestern area of Zhucheng in Jiaolai Basin,which was located in Jiaodong Peninsula,eastern China.Many types of brittle,plastic and liquefied soft-sediment deformation structures were found including load structure,ball-pillow structure,injection structure(flame structure),liquefied deformation,liquefied vein,mixed plunge structure,minor earthquake fault. These deformation structures were typically formed by coarse sediments during palaeoearthquake event.Multi-bed soft-sediment deformation interclated with non-deformed beds,which indicate the earthquakes of the Late Cretaceous in Zhucheng were frequent,multi-stage,periodic and of strong-weak changing.Large scale dinosaur(hadrosaurs)fossils were found in coarse sediments from flood plain and debris flows were mainly from the Lower Cretaceous Laiyang and Qingshan Formations in the southern margin of the basin.Dinosaur fossils buried layer among the structural deformation layers of multi-layer palaeoearthquake soft-sediment deformation may be related with the sudden,strong energetic seismic events which lead to the mud-rock flow burying large scale dinosaur skeletons.

Key words: soft-sediment deformation structure, palaeoearthquake, dinosaur fossil burial, Upper Cretaceous, Zhucheng in Shandong Province

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