满洲里—额尔古纳地区岩浆作用及其大地构造意义 |
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引用本文: | 吕志成,魏存第,段国正,郝立波,李殿超.满洲里—额尔古纳地区岩浆作用及其大地构造意义[J].矿物岩石,2001,21(1):77-85. |
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作者姓名: | 吕志成 魏存第 段国正 郝立波 李殿超 |
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作者单位: | 1. 长春科技大学,中国科学院 2. 长春科技大学, |
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基金项目: | 原地矿部定向基金项目! (地科定 :95 -0 1),国家攀登计划预选项目! (95预 -3 9) |
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摘 要: | 对满洲里-额尔古纳地区不同时代岩浆岩的地质,地球化学特征进行了初步研究,研究表明晚元古代花岗岩具S型花岗岩或地壳改造型花岗岩特征,形成于同碰撞造山环境,加里东早期花岗岩具I型,科迪勒拉I型或ACG特征,代表活动大陆边缘构造属性,加里东晚期花岗岩具S型或地壳改造型特征,代表陆-陆碰撞造山环境,加里东期花岗岩记录了多宝山-牙克石-伊尔施陆间洋壳消减和闭合的过程,海西晚期花岗岩属富碱低钙钙碱性岩石,具S型花岗岩或CPG,KCG花岗岩特征,形成于碰撞后构造环境,中生代早期岩 岩形成于蒙古--鄂霍茨克残余洋“剪刀式”闭合所造成的张性似裂谷环境,中生代晚期岩浆岩形成于挤压环境。
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关 键 词: | 花岗岩 地球化学 构造环境 满洲里-额尔古纳地区 岩浆作用 大地构造 |
文章编号: | 1001-6872(2001)01-0077-85 |
MAGMATISM AND ITS TECTONIC SIGNIFICANCE IN THE MANZHOULI-E'ERGONA REGION |
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Institution: | 2 Changchun University of Science and Technolo |
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Abstract: | Based on the geological and geochemical studies of magmatite in the different period from the Manzhouli-E'erguna region, it is suggested that the Later Proterozoic granitoids, which is characterized by S-type granitoids or crust-reconstructed granite type in south of China,were associated with a collision geodynamic environment. The Early Caledonian granitoids, showing characteristics of I-type granitoids, Cordilleran I-type granitoids or low-K, high-Ca amphibole-bearing calc-alkaline granitoids (ACG),were associated with an active continental margin and reflected the subduction of oceanic crust during the Caledonian period. The Later Caledonian granitoids, which is characterized by S-type granitoids or crust-reconstructed granite type in south of China,were associated with a collision between two continents. The magmatism of the Caledonian recorded the history of subduction of Duobaosan-Yakeshi-Yiershi intercontinental ocean. The Later Hercynian granitoids, which are similar to S-type, cordierite bearing-peraluminous granitoids (CPG) or K-rich calc-alkaline granitods (KCG), revealed a post-collision geodynamic environment. The Early Mesozoic magmatite developed on the tensional background caused by closing of Mongolia-Ehucike Residual Ocean in scissors form. The Later Mesozoic magmatite formed in compression background. |
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Keywords: | granitoids geochemistry tectonic environment Manzhouli-E'erguna region |
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