| 内蒙古贺根山地区早白垩世花岗斑岩时代、成因及其地质意义 |
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| 引用本文： | 王成,任利民,张晓军,余国飞. 内蒙古贺根山地区早白垩世花岗斑岩时代、成因及其地质意义[J]. 地质通报, 2018, 37(10): 1882-1894 |
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| 作者姓名： | 王成 任利民 张晓军 余国飞 |
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| 作者单位： | 新疆地质调查院, 新疆 乌鲁木齐 830000,中国地质大学(武汉)地球科学学院, 湖北 武汉 430074,中国地质大学(武汉)资源学院, 湖北 武汉 430074,湖北省地质局第一地质大队, 湖北 黄石 435100 |
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| 基金项目： | 中国地质调查局项目《内蒙古1∶5万硝泡子（L50E018011）等5幅区域地质矿产调查》（编号：1212011220448） |
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| 摘 要： | 贺根山花岗斑岩位于华北板块和西伯利亚板块结合部位,锆石~(206)Pb/~(238)U年龄加权平均值为137.6±1.6Ma,为早白垩世岩浆活动的产物。地球化学特征表现为主量元素总体富硅,且有较高的分异指数(DI)及碱/铝(NK/A)、Fe_2O/FeO值,较低的TFe、Ti、Mg、Ca和P含量;微量元素蛛网图则表现为富集大离子亲石元素Rb、Th、U,弱富集轻稀土元素La,Ce,明显亏损高场强元素Nb、Ba和Sr、Ti。稀土元素配分图表现为相对富集轻稀土元素、亏损重稀土元素,轻、重稀土元素分异较大、重稀土元素曲线较平坦的右倾型特征。综合分析认为,贺根山花岗斑岩属于高分异弱过铝质高钾钙碱性系列的I型花岗岩,其源区物质可能为来自高钾、正常水含量的长英质陆壳岩石物质。花岗斑岩成因可能是晚古生代末—中生代初古亚洲洋闭合引起的一系列板块碰撞作用(包括蒙古-鄂霍次克洋闭合),使造山后期地壳逐渐增厚并发生重力垮塌,导致构造环境由挤压转变为伸展,同时受古太平洋板块西向俯冲影响的结果。
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| 关 键 词： | 花岗斑岩 锆石U-Pb年龄 地球化学特征 构造背景 贺根山 |
| 收稿时间： | 2017-12-22 |
| 修稿时间： | 2018-03-05 |
Ages, origin and geological implications of Early Cretaceous granite porphyry in Hegen Mountain, Inner Mongolia |
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| WANG Cheng,REN Limin,ZHANG Xiaojun and YU Guofei. Ages, origin and geological implications of Early Cretaceous granite porphyry in Hegen Mountain, Inner Mongolia[J]. Geologcal Bulletin of China, 2018, 37(10): 1882-1894 |
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| Authors: | WANG Cheng REN Limin ZHANG Xiaojun YU Guofei |
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| Affiliation: | Xinjiang Geological Survey Academy, Urumqi 830000, Xinjiang, China,School of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China,Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China and No.1 Geological Party of Hubei Geological Bureau, Huangshi 435100, Hubei, China |
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| Abstract: | Zircon U-Pb age of granite-porphyry in Hegen Mountain located in the conjunction of the North China plate and the Siberia plate is 137.6±1.6Ma, suggesting that the rockswere formed by magmatic evolution during Early Cretaceous. The geochemical data indicate that major elements are characterized by enrichment of Si,higher DI and NK/A as well as Fe2O/FeO ratios. The trace element spider diagram indicates that graniteporphyry is relatively rich in Rb,Th,U,slightly enriched in light rare earth elements La, Ce,and depleted in high field strength elements such as Nb,Ba, Sr and Ti, while the distribution model of REE is right oblique, exhibiting relative LREE-enrichment and HREE-depletion,and the HREE curve is flat. These results suggest that the granite porphyry is attributed to high differentiated metaluminous-weakly peraluminous high calc-alkaline series,being typical I-type granite. The source materials might have come from crustal felsic rocks with high K and normal water content. The formation of the granite porphyry may be related to the process from the extrusion to extension resulting from the lithosphere thinning after plates collision (including Mongolia-Okhotsk Ocean) with the closure of Paleo-Asian Ocean during the Late Paleozoic to the Early Mesozoic. It was also affected by the westward subduetion of the Paleo-Pacific Ocean. |
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| Keywords: | granite porphyry zircon U-Pb age geochemical characteristics tectonic background Hegen Mountain |
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