内蒙古四子王旗黑脑包岩体年代学与地球化学特征及其构造演化

熊光强; 赵洪涛; 刘敏; 张达; 王浩然; 王忠

内蒙古四子王旗黑脑包岩体年代学与地球化学特征及其构造演化

熊光强^1,,
赵洪涛¹,
刘敏¹,
张达^1, ,,
王浩然¹,
王忠²

1.
中国地质大学地球科学与资源学院, 北京 100083
2.
内蒙古地质调查院, 呼和浩特 010020

基金项目:

地质调查项目"中蒙边境东段深部结构及成矿条件对比研究" 1212011085490

详细信息

作者简介:
熊光强(1988-), 男, 中国地质大学(北京)硕士研究生, 构造地质学专业。E-mail:xgq_1201@163.com

通讯作者:
张达, E-mail:zhangda@cugb.edu.cn

中图分类号: P585.3;P588.12
计量
- 文章访问数: 158
- HTML全文浏览量: 40
- PDF下载量: 8
- 被引次数: 0
出版历程
- 收稿日期: 2013-01-26
- 刊出日期: 2013-06-28

GEOCHRONOLOGY AND GEOCHEMISTRY OF THE HEINAOBAO PLUTON IN SIZIWANGQI, INNER MONGOLIA AND ITS TECTONIC EVOLUTION

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geological Survey of Inner Mongolia, Hohhot 010020, China

摘要

摘要: 内蒙古四子王旗黑脑包岩体位于华北板块北缘早古生代增生造山带，主要由花岗闪长岩和花岗斑岩组成。对花岗闪长岩进行La-ICP-MS锆石U-Pb定年，获得四子王旗黑脑包侵入岩体的2个侵位年龄为407.4±4.7 Ma和268.0±2.7 Ma，分别代表洋陆俯冲事件以及陆陆碰撞事件年龄。岩石地球化学数据显示，四子王旗黑脑包岩体属钙碱性系列，逐步向低钾拉斑系列靠近，并且亏损高场强元素。同位素地质年龄及地球化学数据表明，样品具有同碰撞花岗岩特征。结合区域大地构造背景认为，四子王旗黑脑包地区主要构造背景为西伯利亚板块与华北板块之间俯冲、碰撞和对接过程，属古亚洲洋构造域，而后期的构造演化还有待进一步研究。
- 四子王旗黑脑包岩体 /
- 兴蒙造山带 /
- 构造演化 /
- 锆石U-Pb定年
Abstract: Heinaobao granitoid in the Siziwangqi area of Inner Mongolia tectonically belongs to Early Paleozoic hyperplasia plate in the northern margin of the North China plate. The granitiod is predominantly of composed of granodiorite and granote porphyry. The La-ICP-MS U-Pb zircon dating method and petrochemical analysis were used to study and understand its formation age and nature. As a result, zircons from granodiorite U-Pb ages of 407.4±4.7 Ma and 268.0±2.7 Ma, the first age represents the one event of ocean-continent subduction and the second age represents the one event of continent-continent collision. Petrochemistry date indicated that the Heinaobao rock in Siziwangqi belongs to the calc-alkaline series, and gradually near to the hypokalemic Tholeiitic series, depleted in high field strength elements. Geochrono logical and petrochemical data implied that the samples had syn-collisional characteristics. Combined with regional tectonic background, the tectonic background of Heinaobao Sizwangqi is the subduction, collision and docking of Siberian plate and North China Plate, it belongs to Paleo-Asian Ocean tectonic domain, while the late tectonic evolution remains to be further research.
- Heinaobao pluton in Siziwangqi /
- Xing'an Mongolian Orogenic /
- tetconic evolution /
- zircon U-Pb dating

HTML全文

图 1 研究区大地构造位置简图和岩体地质简图

Figure 1. Tectonic location and geological map of the study area

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图 2 黑云母花岗岩中本巴图组捕掳体

Figure 2. The layer xenoliths of the biotite granite

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图 3 硅化破碎带

Figure 3. Silicified broken belt

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图 4 黑云母花岗岩显微特征

Figure 4. Microscopic characteristics of the biotite granite

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图 5 黑脑包岩体锆石样品阴极发光图

Figure 5. CL images of zircons from the Heinaobao pluton

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图 6 黑脑包岩体锆石U -Pb谐和图

Figure 6. Concordia diagrams of U-Pb ages of zirconsfrom the Heinaobao pluton

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图 7 黑脑包岩体TAS图

Ir—Irvine分界线，上方为碱性，下方为亚碱性

Figure 7. TAS diagram of for the heinaobao pluton

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图 8 SiO₂-AR图

AR=(Al₂O₃+CaO+Na₂O+K₂O)/ [(Al₂O₃+CaO)-(Na₂O+K₂O)]

Figure 8. The diagram of SiO₂-AR

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图 9 AFM图解

Figure 9. The diagram of AFM

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图 10 K₂O-SiO₂图解

Figure 10. The diagram of K₂O-SiO₂

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图 11 K₂O-Na₂O图

Figure 11. The diagram of K₂O-Na₂O

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图 12 A/NK-A/KNC图

A/KNC=Al₂O₃/(CaO+Na₂O+K₂O); A/NK=Al₂O₃/(Na₂O+K₂O)

Figure 12. The diagram of A/NK-A/CNK

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图 13 黑脑包岩体微量元素原始地幔标准化蛛网图

Figure 13. Primative mantle-normalized trace element patterns of the Heinaobao pluton

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图 14 稀土元素球粒陨石标准化分布型式图

Figure 14. Chondrite-normalized REE distribution patterns of the Heinaobao pluton

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图 15 黑脑包岩体构造环境判别图解

Syn-COLG—同碰撞花岗岩；VAG—火山弧花岗岩；ORG—洋中脊花岗岩；WPG—板内花岗岩

Figure 15. Discrimination diagrams for tectonic settings of the Heinaobao pluton

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图 16 Rb/10-Hf-Ta^*3构造环境判别图

Figure 16. Discrimination diagram for tectonic settings of Rb/10-Hf-Ta^*3

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图 17 R1-R2图

Figure 17. The diagram of R1-R2

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表 1 黑脑包岩体锆石U-Pb同位素测年分析结果

Table 1. U-Pb isotopic compositions of zircons from the Heinaobao pluton

表 2 黑脑包岩体主量元素分析结果

Table 2. Composition of major elements of samples from the Heinaobao pluton

表 3 黑脑包岩体稀土及微量元素分析结果

Table 3. Composition of trace elements of samples from the Heinaobao pluton

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