武夷山成矿带浙江段成矿物质来源铅同位素证据
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摘要
在区域地质特征研究的基础上,本文通过武夷山成矿带浙江段22组变质基底、29组岩浆岩以及5个典型矿床矿石铅同位素数据分析表明:区内变质岩铅同位素具有明显上地壳源特征,不同时期岩浆岩铅同位素特征各有差异,但整体以上地壳源铅、造山带混合铅为主。研究区典型矿床的矿石铅同位素组成以造山带(混合)铅为主,部分有更深源(下地壳或地幔)铅的参与。另外,矿石铅与燕山期岩浆岩铅同位素组成相近,燕山期岩浆作用可能为区域成矿主控因素,并提供了最主要的成矿物质。
Based on the geological characteristics of the Zhejiang section of the Wuyishan metallogenic belt, we selected 22 sets of metamorphic basement, 29 sets of magmatic rocks, and 5 typical deposits for Pb isotope analysis. We find that the metamorphic rocks in this area have clear Pb isotope characteristics indicating an upper crustal source. In comparison, the Pb isotopic characteristics of magmatic rocks vary over different periods, all Pb sources are dominated by upper crust or orogenic belts(mixed) compositions. Typical deposits in this area are dominated by orogenic belt, i.e., mixed, Pb isotopes, with some involvement from deeper sources, i.e., the lower crust or mantle. The Pb isotopic compositions of the deposits and Yanshanian magmatic rocks are similiar. A hydrothermal system, primarily in the Yanshan period, is both the main controlling factor on mineralization and main source of metallogenic material in the region.
Based on the geological characteristics of the Zhejiang section of the Wuyishan metallogenic belt, we selected 22 sets of metamorphic basement, 29 sets of magmatic rocks, and 5 typical deposits for Pb isotope analysis. We find that the metamorphic rocks in this area have clear Pb isotope characteristics indicating an upper crustal source. In comparison, the Pb isotopic characteristics of magmatic rocks vary over different periods, all Pb sources are dominated by upper crust or orogenic belts(mixed) compositions. Typical deposits in this area are dominated by orogenic belt, i.e., mixed, Pb isotopes, with some involvement from deeper sources, i.e., the lower crust or mantle. The Pb isotopic compositions of the deposits and Yanshanian magmatic rocks are similiar. A hydrothermal system, primarily in the Yanshan period, is both the main controlling factor on mineralization and main source of metallogenic material in the region.
引文
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