| 陶平,陈建书,陈启飞.贵州华力西至印支旋回构造演化与区域成矿规律[J].贵州地质,2025,42(1):1-9, 39 |
| 贵州华力西至印支旋回构造演化与区域成矿规律 |
| Tectonic Evolution and Regional Metallogenic Regularity of Varissian Cycle to Indosinian Cycles in Guizhou |
| 投稿时间：2024-11-09 |
| DOI： |
| 中文关键词: 华力西旋回 印支旋回 构造演化 成矿系列 成矿规律 贵州 |
| 英文关键词:Varissian cycle Indosinian cycle tectonic evolution Metallogenic series Metallogenic regularity Guizhou Province |
| 基金项目:中国矿产地质志项目(编号:DD20221695、DD20190379、DD20160346)资助 |
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| 中文摘要: |
| 以《中国矿产地质志·贵州卷》研究项目为依托，在前人研究基础上，进行了贵州华力西至印支构造旋回构造演化及区域成矿规律的系统研究。认为在该构造旋回，随着构造动力从离散(裂解)向汇聚(造山)发展，盆地类型从陆内裂陷(谷)盆地转化为被动大陆边缘盆地，再转化为板内结合带压陷前陆盆地，从而形成了各时期特有的地质建造及多种矿产。这些矿产在特定的地质建造中呈现出有序分布规律。在此基础上，建立并论述了矿床成矿系列及亚系列。这些成果进一步揭示了贵州该旋回中的区域成矿规律。 |
| 英文摘要: |
| Based on the ‘Guizhou Volume of Mineral Geology of China’ research project，based on previous studies，a systematic study on the tectonic evolution and regional metallogenic regularity of the Varissian to Indosinian tectonic cycle in Guizhou was carried outIt is believed that in this tectonic cycle，with the development of tectonic dynamics from dispersion (fragmentation) to convergence (orogeny)，the basin type changed from intracontinental rift (valley) basin to passive continental margin basin，and then to intracontinental conjunctive zone depressions foreland basin，thus forming the unique geological formations and a variety of minerals in each periodThese minerals show an orderly distribution law in the specific geological constructionOn this basis，the metallogenic series and sub-series of the deposit are established and discussedThese results further reveal the regional metallogenic regularity of this cycle in Guizhou |
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