拉萨地块和羌塘地块多个二叠纪基性岩及一个古特提斯海山的初步古地磁结果:对模拟东冈瓦纳晚古生代裂解的暗示
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引用本文:Diane CHUNG,Jason R. ALI,Jonathan C. AITCHISON.2012.拉萨地块和羌塘地块多个二叠纪基性岩及一个古特提斯海山的初步古地磁结果:对模拟东冈瓦纳晚古生代裂解的暗示[J].地球学报,33(s1):8.
DOI:10.3975/cagsb.2012.s1.05
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作者单位E-mail
Diane CHUNG Department of Earth Sciences, University of Hong Kong chungd@hku.hk 
Jason R. ALI Department of Earth Sciences, University of Hong Kong  
Jonathan C. AITCHISON School of Geosciences, University of Sydney  
中文摘要:Detachment of the sliver-like Cimmerian terrane from eastern Gondwana in the Early Permian triggered mafic volcanism in many parts of the rift zone. To understand this tectonic episode we have carried out paleomagnetic investigations on mafic volcanic for-mations that were erupted on key terranes that now form part of Tibet. Specifically, we will present data from sections near Lhasa City (central Lhasa block) and Tuotuohe (central Qiangtang Block) as well as near Gyanyima (Paleotethyan sea-mount) that was emplaced onto the floor of Palaeotethys during the Late Permian. Paleomagnetic plots from each location will be used for tectonic calculations. Our new data will be used to evaluate regional scale models con-cerned with how the Cimmerian terranes in southern and SE Asia (from Iran-Tibet-SW China-Myanmar- Thailand-Sumatra) formerly abutted eastern Gond-wana.
中文关键词:Paleomagnetism  mafic units  Permian  Lhasa Block  Qiangtang Block  Gyanyima
 
Preliminary Paleomagnetic Results from Various Permian Mafic Units on the Lhasa and Qiangtang Blocks, plus a Paleotethyan Sea-mount: Implications for Modeling Eastern Gondwana’s Late Paleozoic Breakup
Abstract:Detachment of the sliver-like Cimmerian terrane from eastern Gondwana in the Early Permian triggered mafic volcanism in many parts of the rift zone. To understand this tectonic episode we have carried out paleomagnetic investigations on mafic volcanic for-mations that were erupted on key terranes that now form part of Tibet. Specifically, we will present data from sections near Lhasa City (central Lhasa block) and Tuotuohe (central Qiangtang Block) as well as near Gyanyima (Paleotethyan sea-mount) that was emplaced onto the floor of Palaeotethys during the Late Permian. Paleomagnetic plots from each location will be used for tectonic calculations. Our new data will be used to evaluate regional scale models con-cerned with how the Cimmerian terranes in southern and SE Asia (from Iran-Tibet-SW China-Myanmar- Thailand-Sumatra) formerly abutted eastern Gond-wana.
keywords:Paleomagnetism  mafic units  Permian  Lhasa Block  Qiangtang Block  Gyanyima
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