| 祁连山蛇绿岩带和原特提斯洋演化 |
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| 引用本文： | 宋述光,吴珍珠,杨立明,苏犁,夏小洪,王潮,董金龙,周辰傲,毕衡哲.祁连山蛇绿岩带和原特提斯洋演化[J].岩石学报,2019,35(10):2948-2970. |
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| 作者姓名： | 宋述光 吴珍珠 杨立明 苏犁 夏小洪 王潮 董金龙 周辰傲 毕衡哲 |
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| 作者单位： | 教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,中国地质大学科学研究院, 北京 100083,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871,教育部造山带与地壳演化重点实验室, 北京大学地球与空间科学学院, 北京 100871 |
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| 基金项目： | 本文受国家自然科学基金项目（41572040、41372060）和国家重点基础研究发展计划（2015CB856105）联合资助. |
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| 摘 要： | 位于阿拉善地块和柴达木地块之间的祁连造山带记录原特提斯洋扩张、俯冲、闭合、大陆边缘增生和碰撞造山的完整过程。从南向北,祁连造山带发育有三条平行排列、不同类型的蛇绿岩带:(1)南部南祁连洋底高原-洋中脊-弧后蛇绿岩混杂带;(2)中部托勒山洋中脊型蛇绿岩带;(3)北部走廊南山SSZ型蛇绿岩带。南部南祁连蛇绿混杂岩带以拉脊山-永靖蛇绿岩为代表,为典型的洋底高原型蛇绿岩,是大洋板内地幔柱活动的产物,形成年龄为525～500Ma;中部托勒山蛇绿岩带沿熬油沟-玉石沟-冰沟-永登一线分布,为大洋中脊型蛇绿岩,蛇绿岩形成年龄为550～495Ma;北部蛇绿岩带包括弧前和弧后两种类型,弧前蛇绿岩以大岔大阪蛇绿岩为代表,形成时代为517～487Ma,反映初始俯冲/弧前扩张到弧后盆地的过程;弧后蛇绿岩以九个泉-老虎山蛇绿岩为代表,为典型的SSZ型蛇绿岩,是弧后扩张的产物,形成时代为奥陶纪(490～445Ma)。三个蛇绿岩带分别代表了新元古代-早古生代祁连洋演化历史不同环境的产物,对了解秦祁昆构造带原特提斯洋的构造演化过程有重要意义。蛇绿岩及弧火山岩的时空分布特征限定了原特提斯洋的俯冲极性为向北消减俯冲。
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| 关 键 词： | 蛇绿岩带 原特提斯洋 洋底高原 弧前-弧后转换 祁连山 |
| 收稿时间： | 2019/4/25 0:00:00 |
| 修稿时间： | 2019/8/1 0:00:00 |
Ophiolite belts and evolution of the Proto-Tethys Ocean in the Qilian Orogen |
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| SONG ShuGuang,WU ZhenZhu,YANG LiMing,SU Li,XIA XiaoHong,WANG Chao,DONG JinLong,ZHOU ChenAo and BI HengZhe.Ophiolite belts and evolution of the Proto-Tethys Ocean in the Qilian Orogen[J].Acta Petrologica Sinica,2019,35(10):2948-2970. |
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| Authors: | SONG ShuGuang WU ZhenZhu YANG LiMing SU Li XIA XiaoHong WANG Chao DONG JinLong ZHOU ChenAo and BI HengZhe |
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| Institution: | MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China,MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China,MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China,Institute of Earth Science, Chinese University of Geosciences, Beijing 100083, China,MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China,MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China,MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China,MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China and MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China |
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| Abstract: | The Qilian Orogen, which lies between the Alashan Block in the north and the Qaidam Block in the south, records the entire tectonic evolution of Proto-Tethys Ocean from its spreading, subduction, closing, marginal accretion to continental collision. There are three different types of parallel ophiolite belts extending in the Qilian Orogen, from south to north, including:(1) the South Qilian ophiolitic complex belt with oceanic plateau-type, MOR-type and backarc-type ophiolites in the south; (2) the Tuoleshan MOR-type ophiolite belt in the middle; and (3) the Zoulangnanshan back-arc-basin (BAB)-type ophiolite belt in the north. The southern oceanic plateau-type ophiolite belt is represented by Lajishan-Yongjing ophiolite, which is a typical ophiolite fragment of oceanic plateau originated from the Cambrian mantle plume activity during ca. 525~500Ma. The middle ophiolite belt extends along Aoyougou, Yushigou, Binggou and Yongdeng, representing the ophiolite complex of the MOR-type oceanic crust with the ages of 550~495Ma. The northern ophiolite belt contains forarc-type and BAB-type ophiolites. The forarc-type ophiolite, represented by the Dachadaban ophiloite, formed in response to the processes from subduction initiation, forearc extension to back-arc basin development during 517~487Ma; the BAB-type ophiolite, represented by the Jiugequan and Laohushan ophiolites, are the SSZ-type ophiolite and the products of back arc basin extension during Ordovician (490~445Ma). The three ophiolite belts are the products formed in different tectonic settings during the history of Qilian Ocean from Neoproterozoic to Early Paleozoic, and thus is of great significance in understanding the tectonic evolution of Proto-Tethys Ocean in Qin(ling)-Qi(lian)-Kun(lun) Orogenic Belt. The timing and distribution of the three ophiolite belts and arc volcanics constrain a northward subduction polarity. |
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| Keywords: | Ophiolite belts Paleo-tethys Ocean Oceanic plateau Transition from forarc to backarc Qilian Mountain |
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