湘南大山腾山岙矿床地质特征、成矿时代及找矿意义

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Zunzun Zhang , Yongyun Ning , Youyue Lu , Jingya Cao , Jianming Fu , Zhuang Zhao , Jian Guo , Liyan Ma , Zhengwei Qin , Jianfeng Li
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引用次数: 8

摘要

腾山坳锡矿床位于南岭大山矿田,是该地区近年来发现的矿床之一。通过LA-MC-ICP-MS锡石U-Pb和白云母40Ar-39Ar同位素定年分析,蚀变花岗岩型锡矿石的年龄分别为156.7±4.3 Ma和151.1±1.5 Ma。这些年龄与细粒二云母二长花岗岩的LA-MC-ICP-MS锆石U-Pb年龄(158.2±1.6 Ma)一致,表明晚侏罗世腾山坳锡矿床存在岩浆作用和成矿作用。进一步论证了该矿床的形成与南岭早燕山期(160 ~ 150 Ma)大规模成岩成矿作用有关。认为晚期细粒二云母(白云母)花岗岩对寻找蚀变花岗岩型锡多金属成矿具有指示意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Geological characteristics and metallogenic age of Tengshan'ao Sn deposit in Dayishan of South Hunan and its prospecting significance

Geological characteristics and metallogenic age of Tengshan'ao Sn deposit in Dayishan of South Hunan and its prospecting significance

The Tengshan'ao Sn deposit, located at the Dayishan ore field, Nanling Range, is one of the recently explored deposits in this region. In this study, LA-MC-ICP-MS cassiterite U–Pb and muscovite 40Ar-39Ar isotopic dating analyses for altered granite-type Sn ores yielded ages of 156.7 ± 4.3 Ma and 151.1 ± 1.5 Ma, respectively. These ages are consistent to the LA-MC-ICP-MS zircon U–Pb age of the fine-grained two-mica monzogranite (158.2 ± 1.6 Ma), indicating a coeval magmatism and mineralization for the Late Jurassic Tengshan'ao Sn deposit. It is further demonstrated that the formation of this deposit is related to the Early Yanshanian (160-150 Ma) large-scale diagenesis and mineralization in Nanling Range. It is suggested that the late-stage fine-grained two-mica (muscovite) granite has an indicative significance for searching the altered granite type Sn polymetallic mineralization.

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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
发文量
20
审稿时长
103 days
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