Petrology of Cr-rich Ophiolitic Chromitites of Bulqiza, Eastern Ophiolitic Belt, Albania

查看全文 作　　者：XIONG [1]Fahui;YANG [1]Jmgsui;Paul T. [1]ROBINSON;Yildirim [2]DILEK;MILUSHI [3]Ibrahim;XU [1]Xiangzhen;ZHANG [1]Zhongming;ZHOU [4]Wenda;CHEN [1]Yanhong;HUANG [5]Zhu;LAI [5]Shengming;ZHANG [5]Lan 机构地区：[1]CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;[2]Department of Geology& Environmental Earth Science 116 Shideler Hall, Miami University Oxford, OH 45056;[3]Institute of Geosciences, Energy, Water andEnvironment, Polytechnic University of TIRANA;[4]Faculty of Earth Sciences, China University ofGeoscience, Wuhan 430074, China;[5]School of Earth Science and Mineral Resources, China University ofGeosciences, Beijing 100083, China 出　　处：《Acta Geologica Sinica(English Edition)》索引2015年第89卷第A02期,共1页 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 profile from the bottom to the top as follows.The 关 键 词：阿尔巴尼亚 蛇绿岩带 铬铁矿石 岩石学 CR 岩石序列 方辉橄榄岩 超镁铁质