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首页> 外文会议>International Symposium of Geological and Mineragenic Correlation in Contiguous Regions of China, Russia and Mongolia; 20031008-11; Changchun(CN) >The Ore-Forming Systems of Continental Margins of Different Ages in the Altai-Sayan Orogenic Area, Russia
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The Ore-Forming Systems of Continental Margins of Different Ages in the Altai-Sayan Orogenic Area, Russia

机译：俄罗斯阿尔泰-萨彦山造山带不同年龄大陆边缘成矿系统

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摘要

The Altai-Sayan orogenic area (ASOA) and metallogenic province, as a part of the global Central-Asian orogenic belt, were formed during long-term development of the Paleoasian Ocean and their continental margins. It is an example of typical polyaccretionary orogenic system. A certain trend is noted in the evolution of ore-forming processes of the ASOA. The early stage of metallogenic development is related to the origin of Paleoasian ocean and destructive processes of Siberian Craton margins in the Early Riphean. The successive accretion of island arcs of various ages and formation of active continental margins in the Early and Middle Paleozoic was of great importance for metallogeny. The postorogenic stages of metallogenic development are related to intraplate geodynamics resulted from the Siberian Permian-Triassic superplume formation, the manifestations of interblock shift movements and intraplate rifting accompanied by mantle and mantle-crust ore-forming systems.There are four main stages of geodynamic and metallogenic development of the Altai-Sayan orogenic area.
机译：作为全球中亚造山带的一部分的阿尔泰-萨彦造山带（ASOA）和成矿省，是在古海洋及其大陆边缘的长期发展过程中形成的。它是典型的多增生造山系统的一个例子。在ASOA的成矿过程的发展中注意到了某种趋势。成矿发展的早期阶段与古里西洋的起源和早期里菲安时期西伯利亚克拉通边缘的破坏过程有关。在古生代初期和中期，不同年龄的岛弧的连续堆积和活跃大陆边缘的形成对成矿意义重大。成矿发育的后造山阶段与西伯利亚二叠系-三叠纪超泥岩形成，板块间移动和板内裂谷伴有地幔和地壳-成矿系统所导致的板内地球动力学有关。阿尔泰-萨彦山造山带成矿作用。

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