| 东疆阿齐山—黄山复合地体的沉积特征 |
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| 引用本文： | 竺国强,马润则.东疆阿齐山—黄山复合地体的沉积特征[J].矿物岩石,1992,12(1):26-37. |
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| 作者姓名： | 竺国强 马润则 |
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| 作者单位： | 成都地质学院，成都地质学院 成都 610059，成都 610059 |
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| 摘 要： | 优地槽型阿齐山—黄山复合地体在石炭纪的沉积特征明显受其边界断裂带的控制。不同阶段各断裂带活动性质,活动强度的差异导致南北两亚地体沉积物成分、厚度的变化。阿齐山—黄山复合地体的演化历史可分为三个阶段,与边界断裂带的相应演化阶段关系密切。
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| 关 键 词： | 复合地体 沉积特征 新疆 |
CHARACTERISTICS OF DEPOSITION OF AQISHAN-HUANGSHAN COMPOSITE TERRANE,THE EASTERN XINJIANG |
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| Zhu Guoqiang Ma Runze.CHARACTERISTICS OF DEPOSITION OF AQISHAN-HUANGSHAN COMPOSITE TERRANE,THE EASTERN XINJIANG[J].Journal of Mineralogy and Petrology,1992,12(1):26-37. |
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| Authors: | Zhu Guoqiang Ma Runze |
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| Abstract: | During Carboniferous period, characteristics of deposition of Aqishan-Huangshan composite terrane that is the eugeosyncline type, are obviously controled by its boundary fault zones. In distinet stages,the differences of the feature and intensity of activity leads to change of composition and thickness of sediments in two subterranes. The history of evolution of Aqishan-Huangshan composite terrane can subdivide to three stages that are closely relative to relevant stages of evolution of the boundary fault zones. |
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| Keywords: | the eastern Xinjiang composite terrane eugeosycline type volcanic rock belt inversion-accretion history of evolution |
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