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《Journal of Stratigraphy》 2016-01
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EARLY PERMIAN FUSULINE ASSEMBLAGES FROM THE ANNANBA SECTION,EASTERN ALTUN MOUNTAINS

CHEN Rui-ming;CHEN Fen-ning;GU Ping-yang;ZHA Xian-feng;DONG Zeng-chan;Xi'an Center of Geological Surey,China Geological Survey;  
The Annanba section is located in eastern Altun,where the Yingebalake Formation outcrops in the Hongliugou-Lapeiquan melange belt as a fault-controlled block.The lower Yingebalake Formation is characterized by bioclastic limestones and contains abundant fusulinids,as well rare brachiopods and corals.In this study,12 fusuline species belonging to 9genera are recovered from bioclastic limestone of the Yingebalake Formation.These fusuline fossils belong to the Sphaeroschwagerina sphaerica-Robustoschwagerina xiaodushanica assemblage zone.Attempts are made to correlate the fusuline assemblage from the Yingebalake Formation with fusuline zones elsewhere,and on this basis of this correlation it is concluded that the Yingebalake Formation at the Annanba section is of Zisong Stage of the Lower Permian.This study provides biostratigraphic constraints on the age of the bioclastic unit of the Yingebalak Formation,and the new data suggest that the Yingebalake Formation is regionally diachronous.
【Fund】: 中国地质调查局基础地质调查项目(1212011121193);; 国家青年基金项目(No.41002063)和(No.41102073)资助
【CateGory Index】: P534.46
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