| 造山带中古海山残片的识别——以拉脊山缝合带青沙山和东沟地质填图为例 |
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| 引用本文： | 付长垒,闫臻,王秉璋,牛漫兰.造山带中古海山残片的识别——以拉脊山缝合带青沙山和东沟地质填图为例[J].地质通报,2021(1). |
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| 作者姓名： | 付长垒 闫臻 王秉璋 牛漫兰 |
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| 作者单位： | 中国地质科学院地质研究所;青藏高原北部地质过程与矿产资源重点实验室/青海省地质调查院;合肥工业大学资源与环境工程学院 |
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| 基金项目： | 国家自然科学基金项目《拉脊山古洋盆初始俯冲的地质记录和时限研究》(批准号:42072266)、《拉脊山增生楔结构、组成与古洋盆重建研究》(批准号:41872241);中国地质调查局项目《中央山系都兰、天水等地区基础地质调查》(编号:DD20190006);中国地质科学院地质研究所统筹科研项目《共和盆地沉积-构造演化》(编号:S2007)。 |
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| 摘 要： | 造山带内海山/洋岛残片的识别是确定古缝合带和古洋盆存在的直接地质证据。祁连造山带被普遍认为是原特提斯洋盆俯冲和闭合的产物,然而南祁连地区是否存在古洋盆长期存在争议。通过对拉脊山关键地段早古生代岩石开展大比例尺地质填图和室内综合研究,在青沙山和东沟地区识别出连续的由洋岛型枕状玄武岩、火山碎屑岩、泥岩、凝灰岩和灰岩组成的火山-沉积组合序列,它们分别呈构造窗和构造残片产出,是拉脊山增生杂岩的重要组成部分,代表中寒武世—早奥陶世原特提斯洋内海山残片。这些海山残片的识别不仅表明拉脊山地区存在早古生代洋盆和缝合带,同时为造山带古洋盆构造演化研究提供了新思路。
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| 关 键 词： | 海山 缝合带 古洋盆 大比例尺地质填图 拉脊山 |
Identification of the relics of paleo-seamount in orogens:A case study from the geological mapping in Qingshashan and Donggou areas within the Lajishan suture zone |
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| FU Changlei,YAN Zhen,WANG Bingzhang,NIU Manlan.Identification of the relics of paleo-seamount in orogens:A case study from the geological mapping in Qingshashan and Donggou areas within the Lajishan suture zone[J].Geologcal Bulletin OF China,2021(1). |
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| Authors: | FU Changlei YAN Zhen WANG Bingzhang NIU Manlan |
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| Institution: | (Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;Key Laboratory of the Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources/Qinghai Geological Survey Institute,Xining 810012,Qinghai,China;Department of Resources and Environment,Hefei University of Technology,Hefei 230009,Anhui,China) |
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| Abstract: | Identification of the relics of seamount/oceanic island in orogens can provide critical geological evidence for the presence of the suture zone and paleo-ocean basin.The Qilian Orogen is widely considered as the product of subduction and closure of the ProtoTethyan Ocean.However,whether there exists a paleo-ocean basin in the South Qilian is still hotly debated.Based on large-scale geological mapping and comprehensive study on the Early Paleozoic rocks in the key area of Lajishan,a successive volcanic-sedimentary sequence composed of OIB-type pillow basalt,pyroclastic rock,mudstone,tuff,and limestone was recognized in the Qingshashan and Donggou areas.The rocks are outcropped as the tectonic slice and tectonic window respectively.The volcanic-sedimentary sequence is the major components of the accretionary complex within Lajishan,and represents the relics of Middle Cambrian to Early Ordovician seamounts within the Proto-Tethyan Ocean.The identification of these relics of seamount not only indicates that there exist Early Paleozoic ocean basin and suture zone in the Lajishan area but also provides a new idea for the study of tectonic evolution of the paleo-ocean basin in orogens. |
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| Keywords: | seamount suture zone paleo-ocean basin large-scale geological mapping Lajishan |
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