Multi-stage Process of the Bulqiza Chromitites, Eastern Ophiolitic Belt, Albania  

作　　者：XIONG Fahui YANG Jingsui Paul T.ROBINSON Yildirim DILEK Ibrahim MILUSHI 

机构地区：[1]CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences [2]Department of Geology& Environmental Earth Science 116 Shideler Hall, Miami University Oxford [3]Institute of Geosciences, Energy, Water and Environment, Polytechnic University of TIRANA

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期245-,共1页地质学报（英文版）

基　　金：funded by grants from Sinoprobe-05-02 from the Ministry of Science and Technology of China;the NSF China (Nos. 40930313, 40921001, 41202036);the China Geological Survey (Nos. 1212011121263, 12120114061801, 2014DFR2127C);project from Institute of Geology, Chinese Academy of Geological Sciences (J1526)

摘　　要：The ultramafic massif of Bulqiza,which belongs to the eastern ophiolitic belt of Albania,is the most important area for metallurgical chromitite ores.The massif consists of a thick(>4 km)rock sequence,with a generalized

关 键 词：Eastern Ophiolitic Belt Multi-stage Process of the Bulqiza Chromitites ROCK Albania 

分 类 号：P618.3[天文地球—矿床学] P588[天文地球—地质学]