东昆仑哈拉森地区花岗岩类岩石成因及地质意义

何成; 王力圆; 田立明; 徐净

doi:10.3799/dqkx.2018.716

东昆仑哈拉森地区花岗岩类岩石成因及地质意义

doi: 10.3799/dqkx.2018.716

何成^1,2,,
王力圆^3, ,,
田立明⁴,
徐净⁵

1.
中国地震局地震研究所, 地震预警湖北省重点实验室, 湖北武汉 430071
2.
武汉地震工程研究院有限公司, 湖北武汉 430071
3.
福州大学紫金矿业学院, 福建福州 350116
4.
江西省地矿局物化探大队, 江西南昌 330201
5.
中国科学院地质与地球物理研究所, 北京 100029

基金项目:

青藏高原矿产调查评价专项项目 1212011220664

国家自然科学基金 41402098

详细信息

作者简介:
何成(1989-), 男, 硕士研究生, 主要从事矿床学及矿床地球化学研究方向

通讯作者:
王力圆, E-mail:wangliyuan030101@163.com

中图分类号: P581
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出版历程
- 收稿日期: 2017-12-18
- 刊出日期: 2018-04-15

Petrogenesis and Geological Implications of Granitoids from Halasen, East Kunlun

He Cheng^{1,2
,},
Wang Liyuan^{3
, ,},
Tian Liming⁴,
Xu Jing⁵

1.
Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China
2.
Wuhan Institute of Earthquake Engineering Co., Ltd., Wuhan 430071, China
3.
College of Zijin Mining, Fuzhou University, Fuzhou 350116, China
4.
Geophysical and Geochemical Exploration Brigade of Jiangxi, Nanchang 330201, China
5.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

摘要

摘要: 哈拉森地区位于东昆仑东段，分布着大量花岗岩，对其研究不仅有助于认识东昆仑造山带在晚古生代-早中生代的构造-岩浆演化历史，而且可以为东昆仑古特提斯洋俯冲时限及洋盆闭合时限提供约束.对区内花岗岩进行了岩石学、年代学以及岩石地球化学分析，结果表明哈拉森地区的钾长花岗岩和细粒二长花岗岩锆石LA-ICP-MS U-Pb年龄分别为239.2±1.7 Ma（MSWD=0.19）和232.4±1.2 Ma（MSWD=0.76），属中三叠世花岗质岩浆作用的产物.岩石主微量元素分析显示该地区花岗岩具有高硅铝、富碱和低钛特征，属于高钾钙碱性到钾玄岩系列的过铝质花岗岩，富集轻稀土元素（LREE）及K、Th、Rb等大离子亲石元素（LILE），明显亏损Nb、Ti、P、Ta等高场强元素（HFSE），具有非常明显的Eu负异常（δEu为0.27~0.65）.哈拉森地区花岗岩具有高分异Ⅰ型花岗岩的特征，是同碰撞背景下幔源岩浆与其诱发地壳物质熔融产生的长英质岩浆在地壳深部混合，随后这一混合岩浆又经过高程度的分异演化形成的，进一步证明东昆仑古特提斯洋的俯冲作用一直持续到早三叠世，至中三叠世才逐渐转入陆内碰撞造山阶段.
- 花岗岩 /
- 地质年代学 /
- 地球化学 /
- 哈拉森 /
- 东昆仑
Abstract: A large amount of granites widely distributes in Halasen area in the East Kunlun Mountains. The study of the granites not only help us to understand the tectono-magmatic evolution history of East Kunlun orogenic belt in the Late Paleozoic and Early Mesozoic, but also provides constraints for the subduction and closed time limit of the Paleo-Tethys Ocean. In this paper, we constrain geochronology and petrogenesis of the Halasen granites by zircon U-Pb dating and geochemical analyses. The LA-ICP-MS U-Pb analyses show that the formation ages of K-feldspar granite and fine-grained monzogranite are 239.2±1.7 Ma (MSWD=0.19) and 232.4±1.2 Ma (MSWD=0.76), respectively, which are the products of the Middle Triassic granitic magmatism. The geochemistry data show that granites are high-potassium calcalkaline-shoshonite, peraluminous rock which is characterized by high silicon and aluminum, enriched alkali, low titanium, as well as enriched light rare earth elements (LREE) and large ion lithophile elements (LILE, e.g., K, Th and Rb), and depleted in high field-strength elements (HFSE, e.g., Nb, Ti, P, and Ta) with obvious Eu negative anomaly (the value of δEu is between 0.27 and 0.65). Halasen granites belong to highly fractionated Ⅰ-type granite. It is suggested that the Halasen granites were most likely derived from parental magma by mixing of depleted mantle-derived magma and induced crustal-melted felsic magma in the deep crust, and then suffered further differentiation during magma ascent. The subduction of the East Kunlun Paleo-Tethys Ocean lasted to the Early Triassic, and the Middle Triassic witnessed the intracontinental collision.
- granite /
- geochronology /
- geochemistry /
- Halasen /
- East Kunlun

HTML全文

图 1 东昆仑东段大地构造位置(a)和香日德地区地质简图(b)

1.第四系；2.上三叠统鄂拉山组；3.下三叠统洪水川组；4.奥陶系-志留系纳赤台群；5.中元古界小庙岩组；6.古元古界金水口群；7.晚海西-印支期钾长花岗岩；8.晚海西-印支期细粒二长花岗岩；9.晚海西期花岗闪长岩；10.加里东期石英闪长岩；11.脆性断层/韧性断层；12.角度不整合；13.河流；14.研究区；15.采样位置；16.样品数据熊富浩(2014).据王学良(2011)修改

Fig. 1. Tectonic location of eastern part of the East Kunlun orogen (a) and simplified geological map of the Xiangride intrusive rocks (b)

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图 2 哈拉森地区花岗岩手标本及镜下照片

a, b.钾长花岗岩；c, d.细粒二长花岗岩.Kfs.钾长石；Pl.斜长石；Bi.黑云母；Qtz.石英

Fig. 2. Specimen photographs and microscopic images of granites in the Halasen area

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图 3 哈拉森地区钾长花岗岩(a)与细粒二长花岗岩(b)锆石阴极发光(CL)图像(单位：Ma)

Fig. 3. Zircon cathodoluminescence (CL) images of moyite (a) and fine-grained monzogranite (b) in the Halasen area

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图 4 哈拉森地区钾长花岗岩(a)与细粒二长花岗岩U-Pb谐和图(b)

Fig. 4. Zircon U-Pb concordia diagrams of moyite (a) and fine-grained monzogranite (b) in Halasen area

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图 5 哈拉森地区花岗岩分类图解

图a底图据Peccerillo and Taylor(1976)；图b底图据Maniar and Piccoli(1989)

Fig. 5. Genetic discrimination diagrams for the Halasen granitoids

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图 6 哈拉森地区花岗岩稀土元素球粒陨石标准化配分图(a)和微量元素原始地幔标准化蛛网图(b)

标准化值据Sun and McDonough(1989)；图例同图 5

Fig. 6. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element diagram (b) for the Halasen granitoids

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图 7 哈拉森地区花岗岩岩石成因类型

图b底图据Whalen et al.(1987)；图例同图 5

Fig. 7. Genetic discrimination diagrams for the Halasen granitoids

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图 9 哈拉森地区花岗岩源区性质判别图解

图a底图据Altherra et al.(2000)；图b~d底图据Douce(1999)；图例同图 5.A.变质泥岩部分熔融；B.变质砂岩部分熔融；C.基性岩(角闪岩)的部分熔融

Fig. 9. Source characteristics discrimination diagrams for the Halasen granitoids

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图 8 哈拉森地区花岗岩结晶分异特征

图例同图 5

Fig. 8. Characteristics of Halasen granitoids resulting from crystallization differentiation

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图 10 哈拉森地区花岗岩构造环境判别图解(a)和R₁-R₂判别图解(b)

图a据Pearce et al.(1984)；图b据Batchelor and Bowden(1985)；图例同图 5.VAG.火山弧花岗岩；syn-COLG.同碰撞花岗岩；WPG.板内花岗岩；ORG.洋脊花岗岩；①地幔分异产物；②板块碰撞前；③板块碰撞后隆起；④造山晚期；⑤非造山；⑥同碰撞；⑦造山期后

Fig. 10. Tectonic setting discrimination diagrams (a) and R₁-R₂ (b) for the Halasen granitoids

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