Hydrogen and Oxygen Isotopic Characteristics of the Fluid Inclusions from the Liangkeshu Iron Deposit in Altay Region, Xinjiang

The Liangkeshu iron deposit in Xinjiang is located in the Kelang basin at the southern margin of Altay. The iron deposit occurs in pegmatite dikes at the contact zone of monzonitic granite and schist of the Middle-Upper Devonian Aletai Formation. Fluid inclusions in quartz from the ore body, which a...

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Bibliographic Details
Main Authors: GENG Xin-xia, JIANG Li-ping, CHAI Feng-mei, DU Jia-shu, LI Yan, GAO Wen-juan, LIU Feng, LV Shu-jun
Format: Article
Language:English
Published: Science Press, PR China 2013-03-01
Series:Yankuang ceshi
Subjects:
Online Access:http://www.ykcs.ac.cn/en/article/id/574731a3-be21-4a1f-af6f-9767ea196254