滇西珠街萤石-锑矿区含矿岩系凝灰岩锆石U-Pb年龄与沉积时代-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

滇西珠街萤石-锑矿区含矿岩系凝灰岩锆石U-Pb年龄与沉积时代

Zircon U-Pb ages and sedimentary times of the tuffs within the ore-bearing sequences at the Zhujie fluorite-antimony ore field in western Yunnan Province

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DOI	10.20086/j.cnki.yskw.2024.0603
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2024, 43(6)
作者	张涵，王维，薛传东*,
作者单位	昆明理工大学地球科学系, 云南昆明 650093
摘要	兰坪盆地是青藏高原东南缘"三江"造山带与扬子地台西缘结合部的重要含矿沉积盆地之一,其西南部的笔架山萤石-锑矿集区的层控热液成矿特点突出,长期备受关注。前人将其含矿岩系与下伏、上覆地层皆归为上三叠统,但缺乏准确的年代学证据,影响了对区域地层格架、构造演化和矿床成因的合理认识。本文对笔架山矿集区北部的珠街萤石-锑矿区含矿岩系开展了系统的野外地质研究,发现矿体主要呈层状、似层状或层间网脉状集中赋存在三合洞组的硅质岩、硅质角砾岩夹晶屑玻屑凝灰岩构成的火山-沉积岩组合(T₃s^3-2)中;上覆麦初箐组(T₃m)碎屑岩中夹多层凝灰岩。锆石U-Pb定年结果显示,T₃s^3-2赋矿凝灰岩的锆石U-Pb平均年龄为239.4 Ma,T₃m凝灰岩夹层的锆石U-Pb平均年龄为252.2 ~ 216.1 Ma,且具有相似的继承锆石年龄谱。结合区域资料分析,区内T₃s^3-2含矿岩系沉积时代应为中三叠世晚期,代表了一套弧火山岩的同期近源沉积;而麦初箐组是晚三叠世弧岩浆岩带隆升剥蚀的充填堆积产物。因而,区内萤石-锑矿床属同火山期的火山热液沉积型矿床,硅质岩与凝灰岩组合是本区及邻区类似矿床重要的找矿突破方向。
Abstract	The Mesozoic Lanping Basin in western Yunnan Province is one of the most important ore-hosting sedimentary basins between the Sanjiang orogenic belt in southeastern Qinghai-Tibet Plateau and the western margin of the Yangtze platform, SW China. The Bijiashan ore concentration area at the southwest part of this basin contains vast stratified fluorite-antimony hydrothermal deposits and occurrences, and always was highly concerned by the academics and industry. The ore-bearing rocks, the underlying and overlying strata were classified into the Upper Triassic strata by local geologists. However, the lack of accurate chronological evidence has seriously affected our understanding of regional stratigraphic framework, tectonic evolution and ore genesis. In this contribution, we have carried out a systematic field geological investigation on the ore-bearing rocks in the Zhujie fluorite-antimony ore field at the north of the Bijiashan ore concentration area. The field geology shows that the main fluorite-antimony ore-bearing horizons of the uppermost member of the Upper Triassic Sanhedong Formation (T₃s^3-2) is mainly composed of crystalline vitreous tuff, siliceous breccias and siliceous rocks, which is a sedimentary-volcaniclastic assemblage, and the orebodies occur in stratiform and/or lenticular shape. The clastic rocks of the overlying Maichujing Formation(T₃m) are also interbedded with multiple layers of lithocrystalline vitreous tuff. The zircon U-Pb dating results show that the weighted average zircon U-Pb age of the ore-hosting crystalline vitreous tuff from the second part of the upper member of the Upper Triassic Sanhedong Formation (T₃s^3-2) is 239.4 Ma, and the weighted average zircon U-Pb age of the lithocrystalline vitreous tuffs from the lower members of the T₃m Formation range from 252.2 Ma to 216.1 Ma, both of which have similar dated age spectra of the inherited zircons. Combined with the analysis data of regional geology, the ore-bearing rocks of the upper member of the Upper Triassic Sanhedong Formation (T₃s³) in the Zhujie ore field deposited at the late Middle Triassic, which represents the proximal volcanic- sedimentary depositions coeval with the arc-volcanism. Whilst the Upper Triassic formations were originated from the filling of uplift and denudation of the arc magmatic rocks, which record multiphase transition of regional basin-range events. Therefore, the known orebodies in the Zhujie fluorite-antimony ore field is a volcanic hydrothermal sedimentary deposit associated with coeval volcanism. The association of siliceous rock and tuff is an important prospecting mark for similar fluorite-antimony deposits in this ore field and adjacent areas with great prospecting potentials.
关键词	凝灰岩；锆石U-Pb定年；中三叠世；珠街萤石-锑矿区；兰坪盆地
KeyWord	tuffs; zircon U-Pb dating; Middle Triassic; Zhujie fluorite-antimony ore field; Lanping Basin
基金项目
页码	1380-1410

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张涵，王维，薛传东*. 滇西珠街萤石-锑矿区含矿岩系凝灰岩锆石U-Pb年龄与沉积时代 [J]. 岩石矿物学杂志. 2024; 43; (6). 1380 - 1410.

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