内蒙古克什克腾旗毛盖吐锡矿点LA-ICP-MS锡石U-Pb年龄及地质意义

蒋斌斌; 邹滔; 祝新友

doi:10.19509/j.cnki.dzkq.2022.0068

内蒙古克什克腾旗毛盖吐锡矿点LA-ICP-MS锡石U-Pb年龄及地质意义

doi: 10.19509/j.cnki.dzkq.2022.0068

蒋斌斌^1,,
邹滔^2, ,,
祝新友²

基金项目:

国家重点研发计划"深地资源勘查开采"重点专项项目所属课题 2017YFC0601305

国家重点研发计划"深地资源勘查开采"重点专项项目所属课题 2017YFC0602403

详细信息

作者简介:
蒋斌斌(1991—)，男，工程师，主要从事成矿规律研究和大比例尺找矿预测。E-mail：jbb_geo@163.com

通讯作者:
邹滔(1983—)，男，高级工程师，主要从事岩石地球化学及矿床学研究工作。E-mail：13436751833@163.com

中图分类号: P618.44
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- 文章访问数: 354
- PDF下载量: 37
- 被引次数: 0
出版历程
- 收稿日期: 2021-06-08

LA-ICP-MS cassiterite U-Pb ages and the geological significance of the Maogaitu Sn ore spot in Hexigten Banner, Inner Mongolia

Jiang Binbin^1
,,
Zou Tao^{2
, ,},
Zhu Xinyou²

摘要

摘要:
毛盖吐锡矿点为北京矿产地质研究院在大兴安岭南段新发现的矿点, 位于内蒙古克什克腾旗境内。矿点地处大兴安岭中南段多金属成矿带, 矿化类型为锡石石英脉型。矿石矿物主要为锡石和少量闪锌矿、方铅矿、黄铜矿以及银的矿物, 脉石矿物主要为石英以及少量的萤石。该矿由于首次发现, 研究程度较低, 关于其矿床成因、成矿时代等规律尚不明确。大兴安岭中南段多金属成矿带上发育多个锡多金属矿床, 目前的研究表明这些锡多金属矿床的成矿年龄多集中在早白垩世, 成因与早白垩世花岗岩相关。为了研究毛盖吐锡矿与区域锡多金属成矿作用的联系, 开展了对毛盖吐锡矿点成矿时代的研究, 本研究选取1件石英脉型锡矿石样品进行LA-ICP-MS锡石U-Pb定年, 获得锡石的²⁰⁷Pb/²⁰⁶Pb-²³⁸U/²⁰⁶Pb谐和年龄为130.2±3.4 Ma(MSWD=2.9), 表明毛盖吐锡矿点形成于早白垩世, 这与区域上主要的锡多金属矿床成矿时代一致, 说明在大兴安岭中南段寻找锡多金属矿床拥有很好的前景。
- 锡石U-Pb年龄 /
- 毛盖吐锡矿 /
- 内蒙古 /
- 大兴安岭中南段
Abstract:
The Maogaitu Sn ore spot in Hexigten Banner, Inner Mongolia is a newly discovered ore spot in the south section of Greater Khingan Range by Beijing Institute of Geology for Mineral Resources. It is tectonically located in the polymetallic metallogenic belt in the south centralsection of Greater Khingan Range, and the mineralization is characterized by cassiterite-quartz veins. Ore minerals of the ores are dominated by cassiterite with trace amounts of sphalerite, galena, chalcopyrite and silver minerals, while gangue minerals are mainly quartz and fluorite. As discovered recently without detailed studies, the genesis and age of the Maogaitu Sn ore spot are not clearly addressed. A number of tin polymetallic deposits are documented to develop in the polymetallic metallogenic belt in the south central section of Greater Khingan Range. The ages of these tin polymetallic deposits are constrained to be mostly around the Early Cretaceous, and to be genetically related to the Early Cretaceous granite. In order to address the relationship of the Maogaitu Sn ore spot with regional metallogeny, we obtained the age of the Maogaitu Sn ore spot by using LA-ICPMS U-Pb isotopic dating of cassiterite from a quartz vein-type tin ore sample. The results show that the sample yields a ²⁰⁷Pb/²⁰⁶Pb-²³⁸U/²⁰⁶Pb concordant age of (130.2±3.4) Ma (MSWD=2.9), similar to the timing of the major tin mineralization event in the region. The new findings imply that the middle and south sections of Greater Khingan Range could be good targets for Sn polymetallic exploration.
- cassiterite U-Pb age /
- Maogaitu Sn deposit /
- Inner Mongolia /
- middle-southern sections of Greater Khingan Range

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图 1 中国东北构造分区简图(a)(据文献[16])和大兴安岭南段地质简图(b)(据文献[3])

Figure 1. A sketch of the geotectonic unit of Northeast China (a) and the southern Great Khingan Range (b)

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图 2 毛盖吐锡矿点地质简图

Figure 2. A simplified geological map of the Maogaitu Sn ore spot

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图 3 毛盖吐锡矿点矿石特征

a.锡石石英脉；b.石英脉型锡矿石；c.石英交代锆石(透射光下单编光照片)；d.石英与锡石共生(反射光下单偏光照片)。Cst.锡石；Q.石英

Figure 3. Ore characteristics of the Maogaitu Sn ore spot

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图 4 毛盖吐矿点锡石背散射(BSE)图像

Figure 4. Backscattered electron(BSE) image of cassiterite from the Maogaitu Sn ore spot

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图 5 毛盖吐矿点锡石U-Pb年龄谐和图(Tera-Wasserburg)

Figure 5. U-Pb concordia diagrams (Tera-Wasserburg) of cassiterite from the Maogaitu Sn ore spot

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表 1 毛盖吐锡矿点LA-ICP-MS锡石U-Pb定年数据

Table 1. Results of LA-ICP-MS cassiterite U-Pb dating of the Maogaitu Sn ore spot

分析点号	同位素比值
分析点号	²⁰⁷Pb/²³⁵U	2σ	²⁰⁶Pb/²³⁸U	2σ	²³⁸U/²⁰⁶Pb	2σ	²⁰⁷Pb/²⁰⁶Pb	2σ
SHY-46-2	0.418 5	0.025 9	0.022 9	0.000 3	43.657 7	1.397 8	0.132 5	0.000 8
SHY-46-3	0.140 5	0.004 5	0.020 5	0.000 2	48.805 1	1.519 5	0.049 7	0.000 4
SHY-46-4	0.141 2	0.004 1	0.020 1	0.000 2	49.753 1	1.547 5	0.050 9	0.000 1
SHY-46-5	0.147 7	0.009 6	0.020 1	0.000 3	49.721 7	1.702 3	0.053 3	0.000 1
SHY-46-6	0.141 2	0.005 8	0.020 1	0.000 2	49.818 9	1.574 4	0.051 0	0.000 6
SHY-46-7	0.148 7	0.008 4	0.019 9	0.000 3	50.356 4	1.723 0	0.054 3	0.000 4
SHY-46-8	0.138 4	0.004 2	0.020 7	0.000 1	48.260 6	1.489 1	0.048 5	0.002 1
SHY-46-9	0.150 4	0.005 1	0.020 6	0.000 2	48.446 2	1.504 9	0.052 9	0.000 1
SHY-46-12	1.277 6	0.164 8	0.034 7	0.003 4	28.794 3	2.970 1	0.266 8	0.000 9
SHY-46-13	2.883 2	0.255 0	0.046 7	0.003 3	21.394 6	1.630 3	0.447 4	0.003 4
SHY-46-14	0.143 9	0.004 1	0.020 8	0.000 2	48.056 5	1.485 8	0.050 2	0.000 3
SHY-46-15	0.104 0	0.032 7	0.020 9	0.000 2	47.890 0	1.532 4	0.036 1	0.000 4
注：测试单位为中国地质大学(武汉)地质过程与矿产资源国家重点实验室；测试方法为激光剥蚀电感耦合等离子体质谱法(LA-ICP-MS)

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表 2 维拉斯托锡多金属矿和毛盖吐锡矿点地质特征对比

Table 2. Comparison of geological characteristics between Weilasituo tin polymetallic deposit and the Maogaitu Sn ore spot

	维拉斯托锡多金属矿床	毛盖吐锡矿点
区域地质背景	黄岗梁-甘珠尔庙多金属成矿带	黄岗梁-甘珠尔庙多金属成矿带
赋矿围岩	锡林郭勒杂岩	二叠系砂岩
矿体形态	主要为脉状	脉状
矿化组合	Sn-Cu-Pb-Zn-Ag	Sn-Cu-Pb-Zn-Ag
矿物组合	锡石、黝锡矿、闪锌矿、方铅矿、黄铜矿、黄铁矿、黄玉、石英、萤石等	锡石、闪锌矿、方铅矿、石英、萤石等
蚀变	云英岩化	云英岩化
成矿岩体	碱长花岗岩	花岗岩
成矿时代	早白垩世	早白垩世

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