ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
燕山褶断带中生代盆地变形-板内变形过程的记录--以下板城、承德-上板城、北台盆地为例
  
关键词:Mesozoic basin  intraplate deformation  Xiabancheng basin  Chengde—Shangbancheng basin  Beitai basin  northern Hebei Province
基金项目:国土资源大调查项目(编号:200213000040、200013000168); 国家自然科学基金重点项目(编号:40132020)
作者单位
徐刚 中国地质科学院地质力学研究所北京100081 
赵越 中国地质科学院地质力学研究所北京100081 
高锐 中国地质科学院地质研究所北京100037 
李秋生 中国地质科学院地质研究所北京100037 
胡健民 中国地质科学院地质力学研究所北京100081 
刘晓文 国土资源部实物地质资料中心河北燕郊065201 
吴海 国土资源部实物地质资料中心河北燕郊065201 
杨富全 国土资源部实物地质资料中心河北燕郊065201 
张拴宏 中国地质科学院地质力学研究所北京100081 
管烨 中国地质科学院地质研究所北京100037 
张季生 中国地质科学院地质研究所北京100037 
白金 中国地质科学院地质研究所北京100037 
匡朝阳 中国地质科学院地质研究所北京100037 
王海燕 中国地质科学院地质研究所北京100037 
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摘要:
Mesozoic Basin Deformation of Yanshan Folded Fault Belt-Records of the Intraplate Deformation Process: A Case Study of Xiabancheng, Chengde-Shangbancheng and Beitai Basins
      This paper discusses the evolution of Mesozoic intraplate orogenesis on the basis of sedimentary records and deformational analysis of three-generation Mesozoic basins in Xiabancheng and Chengde area of Yanshan folded fault belt. Three Mesozoic basins are from old to young Triassic—Middle Jurassic Xiabancheng basin, late Middle Jurassic—Late Jurassic Chengde—Shangbancheng basin and Early Cretaceous Beitai basin, with their sedimentary sequence composed of three regional Mesozoic structure layers. Xiabancheng basin is a reversed syncline with its sedimentary sequence composed of fluvial alluviation facies; Chengde—Shangbancheng basin is a dissymmetric syncline with its sedimentary sequence composed of volcanic alluviation facies; Beitai basin is a trapped syncline with its sedimentary sequence composed of volcanic sedimentary facies. The deformation of three-generation Mesozoic basins is inconsistent, respectively belonging to different tectonic layers of complicated deformation in their original places, and the older strata of complicated fold deformation are obviously covered by the new basin. Two regional angular unconformities separating the three tectonic layers are before 160 Ma and before 135 Ma in age, corresponding to“Unconformity A” and “Unconformity B” episodes of regional Yanshanian movement.
XU Gang,ZHAO Yue,GAO Rui,LI Qiu-sheng,HU Jian-min,LIU Xiao-wen,WU Hai,YANG Fu-quan,ZHANG Shuan-hong,GUAN Hua,ZHANG Ji-sheng,BAI Jin,KUANG Chao-yang,WANG Hai-yan.2006.Mesozoic Basin Deformation of Yanshan Folded Fault Belt-Records of the Intraplate Deformation Process: A Case Study of Xiabancheng, Chengde-Shangbancheng and Beitai Basins[J].Acta Geoscientica Sinica,27(1):1-12.
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