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

作　　者：XIONG Fahui YANG Jmgsui Paul T. ROBINSON Yildirim DILEK MILUSHI Ibrahim XU Xiangzhen ZHANG Zhongming ZHOU Wenda CHEN Yanhong HUANG Zhu LAI Shengming ZHANG 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)》2015年第A02期102-102,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 profile from the bottom to the top as follows. The tectonite sequence composed mainly of harzburgites with subordinate intercalations of dunites,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 tectonite sequence composed mainly of harzburgites with subordinate intercalations of dunites,

分 类 号：P588[天文地球—岩石学] P618.3[天文地球—地质学]