ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
晚古生代冈瓦纳的演化长逾13500 km的基墨利超级地体的裂离及其向亚洲的漂移
  
关键词:Cimmerian terrane  Paleomagnetism  Baoshan Block  Sibumasu Block
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作者单位E-mail
Jason R. ALI Department of Earth Sciences, University of Hong Kong jrali@hku.hk 
Jonathan C. AITCHISON School of Geosciences, University of Sydney  
Haz M.C. CHEUNG Department of Earth Sciences, University of Hong Kong  
Sam S.Y.CHIK Department of Earth Sciences, University of Hong Kong  
SUN Ya-dong Faculty of Earth Sciences, China University of Geosciences
School of Earth and Environment, University of Leeds 
 
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摘要:
Late Paleozoic Development of Gondwana: Detachment of the >13,500-km-Long Cimmerian Super Terrane and Its Drift to Asia
      The Cimmerian terrane forms an almost unbroken chain stretching >13,500 km, from central southern Europe to western Indonesia, via SE Europe, the Middle East, Afghanistan, Tibet, SW China and Myanmar. Ar-guably, it is Earth’s most spectacular example of a “sliver” terrane, dwarfing in size more recently devel-oped examples, for instance the Palawan Block in the western Philippines, and the Lord Howe Rise in the Tasman Sea. The presentation will first outline the in-triguing geological features associated with this unique tectonic entity. Following that, recently obtained results following paleomagnetic investigations of two lower Permian rift-related basalt suites will be summarized (Abor Volcanics in northeastern India and Woniusi Ba-salts in Yunnan, China). The two studies are part of a larger programme of ongoing research aimed at deducing (I) the geodynamic configuration that generated the un-usual rifting system, and (II) exactly how Cimmeria fit-ted against Gondwana prior to its dispersal in the Early Permian. The critical unit is Baoshan, which we fit against Gondwana within a narrow longitudinal belt close to where northern India and northwestern Australia were once in close proximity (Fig. 1). Furthermore, we suggest that Sibumasu lay to directly the east, offshore of Australia; Qiangtang and Lhasa almost certainly sat to the west (off northern Greater India-SE Arabia), but we are uncertain as to their exact configuration. Our findings will be compared with several rather different models that have been published in recent years. The new pa-leomagnetic constraint highlights the flexibility authors currently have in reconstructing the region, principally because of the overall lack of similar high-quality data from the various blocks. We explain how new data could resolve these ambiguities, thereby offering more robust explanations for eastern Gondwana’s late Paleozoic de-velopment.
Jason R. ALI,Jonathan C. AITCHISON,Haz M.C. CHEUNG,Sam S.Y.CHIK,SUN Ya-dong.2012.Late Paleozoic Development of Gondwana: Detachment of the >13,500-km-Long Cimmerian Super Terrane and Its Drift to Asia[J].Acta Geoscientica Sinica,33(s1):2-3.
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