| 武当地区新元古代岩浆岩地球化学特征及其对南秦岭晋宁期区域构造性质的指示 |
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| 引用本文： | 凌文黎,程建萍,等.武当地区新元古代岩浆岩地球化学特征及其对南秦岭晋宁期区域构造性质的指示[J].岩石学报,2002,18(1):25-36. |
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| 作者姓名： | 凌文黎 程建萍 |
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| 作者单位： | 中国地质大学地球科学学院,武汉,730074 |
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| 基金项目： | 研究获国家自然科学基金项目(49873010,49794043)，国土资源部科技项目(20001010203)，西北大学大陆动力学教育部重点实验室开放课题基金资助. |
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| 摘 要： | 对南秦岭武当地区武当群火山岩、基性侵入岩墙群和耀岭河群火山岩系统的元素和Nd同位素地球研究化学研究表明，武当群火山岩为形成于约1．0－0．9Ga的新元古代陆缘岛弧火山岩，而耀岭河群火山岩与武当地区基性侵入岩墙群为0．82－0．78Ga形成的大陆裂谷型同源岩浆岩；分别可与扬子克拉通北缘西乡群和南秦岭陕西境内的镇安磨沟峡火山岩、扬子克拉通北缘的火地垭群铁船山组碱性火山岩和望江山基性侵入岩群相对比，揭示出南秦岭与扬子克拉通北缘于晋宁期属统一的陆块。扬子克拉北缘和南秦岭大量的新元古代岩浆岩所具有的1．2－0．9GaNd同位素模式年龄和较高的εNd正值特征表明，晋宁期是扬子克拉通地壳增生和大陆岩石圈演化的重要时期之一。
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| 关 键 词： | 武当地区 晋宁期岩浆岩 高秦岭 扬子克拉通 统一陆块 |
| 修稿时间： | 2001年4月11日 |
Geochemical features of the Neoproterozoic igneous rocks from the Wudang region and their implications for the reconstruction of the Jinning tectonic evolution along the south Qinling orogenic belt. |
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| LING WenLi,CHENG JianPing,WANG XingHua and ZHOU HanWenFaculty of Earth Sciences,China University of Geosciences,Wuhan,China.Geochemical features of the Neoproterozoic igneous rocks from the Wudang region and their implications for the reconstruction of the Jinning tectonic evolution along the south Qinling orogenic belt.[J].Acta Petrologica Sinica,2002,18(1):25-36. |
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| Authors: | LING WenLi CHENG JianPing WANG XingHua and ZHOU HanWenFaculty of Earth Sciences China University of Geosciences Wuhan China |
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| Abstract: | A comprehensive study of geochemistry was made on a series of the Jinning period (1. 0~0. 75Ga) igneous rocks from the Wudang region, South Qinling Orogenic belt (SQOB). It shows that the volcanics of Wudang Gp, aged ca. 1. 0-0. 95 Ga, have the affinities of arc magmas , and could be compared, in terms of geochemistry and ages, with those from the adjacent Xixiang Gp located at the northern margin of the Yangtze craton (NMYC) and Mogouxia volcanics from SQOB in Shanxi province. Yaolinghe volcanics and Wudang mafic dikes, which emplaced into both Wudang and Yaolinh Gps, share the magma characteristics of the continental rift, and are thought to be the equivalents of Tiechanshan alkaline volcanics and Wangjiangshan mafic swarms from the NMYC, which were radiometriolly dated as ca. 0. 82-0. 78 Ga. The similar experience in tectonic evolution from subduction zone transforming to continental rifting in the two regions indicates that the NMYC and SQOB belong to a unigue continental block, even though the later one is earmarked of strong deformation due to the Phanerozoic orogeny. TDM model ages of ca. 1. 2~0. 9 Ga and high positive ENd values for the Neoproterozoic igneous rocks of the Wudang region demonstrate that the Jinning events played extremely significant role in both crust growth and lithosphere evolution of the regiona. |
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| Keywords: | Wudang region Jinning igneous rocks South Qinling orogenic belt Yangtze craton unigue continental block |
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