Discovery of Carboniferous Gabbro in the Haernuer Ophiolite around Nalati  

作　　者：ZENG Linggao ZHU Guanghui WU Peng 

机构地区：[1]No.9 Geological Party,Bureau of Geo-exploration and Mineral Development of Xinjiang,Urumqi 830000,China [2]Faculty of Geosciences and Resources,China University of Geosciences,Beijing 100083,China [3]State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China

出　　处：《Acta Geologica Sinica(English Edition)》2021年第5期1779-1781,共3页地质学报（英文版）

基　　金：financially supported by the Geological Exploration Foundation of the Xinjiang Uygur Autonomous Region(Grant No.T15-1-LQ12)。

摘　　要：Objective Ophiolite constitutes an important record of the history of the geological evolution of orogenic belts.There are four important Paleozoic ophiolite(mélange)zones in the Yining Block,northwestern China:northern Tianshan;northern margin of Middle Tianshan;southern margin of Middle Tianshan;and southern Tianshan in the Tianshan orogenic zone.

关 键 词：zone. TIANSHAN MIDDLE 

分 类 号：P587[天文地球—岩石学] P542[天文地球—地质学]