Toward a stepwise Kwangsian Orogeny  

作　　者：CHEN Xu FAN JunXuan CHEN Qing TANG Lan HOU XuDong 

机构地区：[1]State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences [2]College of Resources and Metallurgy, Guangxi University

出　　处：《Science China Earth Sciences》2014年第3期379-387,共9页中国科学（地球科学英文版）

基　　金：supported by Chinese Academy of Sciences(Grant No.KZCX2-EW-111);the State Key Laboratory of Palaeontology and Stratigraphy and Key Laboratory of Economic Stratigraphy and Paleogeography(Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences);National Natural Science Foundation of China(Grant No.41272042)

摘　　要：The Kwangsian Orogeny originated along the southeast coast of China and stepwise developed in a northwest direction.It includes two stages,a long locally varying uplift from the Late Ordovician to the early Silurian and a finally tectonic movement near the Silurian and Devonian transition.The Kwangsian uplift event shows a stepwise delay northwestwards from the southeastern coast area in Nemagraptus gracilis Biozone(Sa1)to the south side of the Xuefeng Mountains in or later than Cystograptus vesiculosus Biozone(R3)to Coronograptus cyphus Biozone(R4).In the southern of Yangtze Platform,the Yichang Uplift was droved by the Kwangsian Orogeny forming a diachronous stratigraphical break through Rhuddanian and Aeronian.The distribution of the early Telychian lower marine red beds indicates a northwestward increase of the Cathaysian Oldland.Stratigraphical evidence may explain why the Kwangsian movement was marked by an angular disconformity during the Pridoli to earliest Devonian interval.The Kwangsian Orogeny originated along the southeast coast of China and stepwise developed in a northwest direction.It includes two stages,a long locally varying uplift from the Late Ordovician to the early Silurian and a finally tectonic movement near the Silurian and Devonian transition.The Kwangsian uplift event shows a stepwise delay northwestwards from the southeastern coast area in Nemagraptus gracilis Biozone（Sa1）to the south side of the Xuefeng Mountains in or later than Cystograptus vesiculosus Biozone（R3）to Coronograptus cyphus Biozone（R4）.In the southern of Yangtze Platform,the Yichang Uplift was droved by the Kwangsian Orogeny forming a diachronous stratigraphical break through Rhuddanian and Aeronian.The distribution of the early Telychian lower marine red beds indicates a northwestward increase of the Cathaysian Oldland.Stratigraphical evidence may explain why the Kwangsian movement was marked by an angular disconformity during the Pridoli to earliest Devonian interval.

关 键 词：uplift stage of the Kwangsian Orogeny Kwangsian movement stepwise initiation of the Kwangsian Orogeny KATIAN Rhuddanian Aeronian 

分 类 号：P542[天文地球—构造地质学]