Chang, Zhaoshan, and Feng, Zhongyan (1998) Albitization of the Kuangshancun intrusion, Southern Taihang Mountains, China. Mineral Deposits, 17 (Supplementary). pp. 623-624.

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Abstract

Based on detailed geological and geochemical investigation, we have established the sequence of the mamatic-hydrothermal events of the Kuangshancun Intrusion. We have estimated the physiochemical conditions of each event. The magmatic-hydothermal processes can be divided into 3 stages: main magmatic stage, late magmatic stage and post magmatic stage. During the late magmatic stage there was interactions between melt, already crystallised rock forming minerals and aqueous phases. The pervasive albitization occurred during the late magmatic stage, as a result of the alteration of rock-forming minerals by magmatic hydrothermal fluids.

Item ID:	35301
Item Type:	Article (Short Note)
ISSN:	0258-7106
Related URLs:	Publisher
Date Deposited:	17 Sep 2014 23:30
FoR Codes:	04 EARTH SCIENCES > 0403 Geology > 040307 Ore Deposit Petrology @ 100%
SEO Codes:	84 MINERAL RESOURCES (excl. Energy Resources) > 8401 Mineral Exploration > 840104 Iron Ore Exploration @ 100%
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