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坦桑尼亚梅拉尼坦桑石矿床地质特征及成因模式

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通过野外实地矿区地质填图,对坦桑尼亚梅拉尼坦桑石矿床的地质背景及矿区矿床地质特征进行详细描述,尤其对矿体及矿物宝石学特征进行了剖析和综述,探讨了宝石成因模式.认为坦桑石形成于约5亿年前的泛非运动,仅产于新元古代莫桑比克变质带的蚀变石墨片麻岩中,属于接触交代成因的矽卡岩矿床,主要受地层岩性和构造变形两个因素控制.
Geological characteristics and its genetic model of tanzanite deposit at Merelani,Tanzania
Through the field geological mapping,the geological setting and its mineralization characteristics for tanzanite deposit at Merelani area,Tanzania are described in details,especially the occurrences of orebodies and characteristics of gemstone are analyzed and reviewed,further its genetic model is discussed preliminarily.It is considered that tanzanite has been formed in the altered graphite gneiss which distributed in the Neoproterozoic Mo-zambique metamorphic belt at proximately 500 Ma when the Pan-African movement was taken place.Being a skarn deposit related to the contact metasomatism,the lithostratigraphic and tectonic deformation are two main controlling factors.

skarngeological characteristicstanzanitegenetic modelMerelani

孙国锋、张明云、闫红圃、张猛、张伟杰、LLOYD Shawarira

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河南省地质研究院,郑州 450001

河南省第二地质勘查院有限公司,郑州 450046

中金国检珠宝玉石质量检验中心有限公司,广东深圳 518020

津巴布韦地质调查局,津巴布韦哈拉雷ZW192201

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矽卡岩 地质特征 坦桑石 成因模式 梅拉尼

河南省地质研究院2023年度地质科技攻关项目

2023-903-XM007-KT03

2024

世界地质
吉林大学 东北亚国际地学研究与教学中心

世界地质

CSTPCD
影响因子:0.769
ISSN:1004-5589
年,卷(期):2024.43(3)