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福建平和东槐叶蜡石矿床地质特征及成因探讨

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平和东槐叶蜡石矿位于政和—大埔断裂带东侧,东山林—桂竹洋北东向断裂带和芦溪—霞寨北西向断裂带的交会处.矿体贮存于晚侏罗世南园组第二段流纹质晶屑凝灰岩中,受北东东向挤压蚀变带控制.在研究矿床地质特征的基础上,通过对比分析矿石与母岩化学成分变化、矿石X射线衍射谱特征,认为该矿床属典型的火山期后构造热液交代型叶蜡石矿床.对该矿床成因进行探讨,为寻找同类矿床提供借鉴.
Discussion on Geological Characteristics and Genesis of Donghuai Pyrophyllite Deposit in Pinghe County,Fujian Province
Donghuai Pyrophyllite Deposit in Pinghe County is located in the east side of Zhenghe-Dapu fault zone,the intersection of Dongshanlin-Guizhuyang north-east fracture zone and Luxi-Xiazhai north-east fracture zone.The ore body is stored in the second section of rhyolitic crystalline tuff of the late Jurassic Nanyuan Formation,which is controlled by the north-east-east extrusion erosion zone.On the basis of studying the geological characteristics of the deposit,through the change of the chemical composition of the ore and the mother rock and and the X-ray diffraction spectra of the ore are compared,it is considered that the deposit belongs to the typical hydrothermal metasomatism type of the leaf wax ore.

pyrophyllitegeological characteristicsgenetic researchDonghuai area of Pinghe country

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福建省闽东南地质大队,泉州,362000

叶蜡石 地质特征 成因探讨 平和东槐

2024

福建地质
福建省地质测绘院

福建地质

影响因子:0.304
ISSN:1001-3970
年,卷(期):2024.43(2)
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