| 安徽沿江地区中生代岩浆岩的基本特点 |
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| 引用本文： | 邢凤鸣,徐祥.安徽沿江地区中生代岩浆岩的基本特点[J].安徽地质,1995(1). |
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| 作者姓名： | 邢凤鸣 徐祥 |
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| 作者单位： | 安徽省地质科学研究所 |
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| 摘 要： | 长江中下游地区是我国著名的中生代铁铜成矿带，成矿与岩浆活动密切相关，沿近东西向的大陆深断裂或裂谷分布，我们称该带的岩浆岩为扬子岩浆岩带。安徽沿江地区处在扬子岩浆岩带的中段，岩石类型齐全，构造面貌比较清楚，最有代表性，是研究该带特点的一个窗口。我们通过近几年的研究，取得了一些新的进展，扼要报导如下。
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| 关 键 词： | 扬子岩浆岩带 特点 安徽 |
Basic Characteristies of the Mesozoic Magmatic Rocks along the Yangize River, ANhui |
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| Xing Fengming, Xu Xiang.Basic Characteristies of the Mesozoic Magmatic Rocks along the Yangize River, ANhui[J].Geology of Anhui,1995(1). |
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| Authors: | Xing Fengming Xu Xiang |
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| Abstract: | The area aiins the Middle-lower Yangtze River is a famous Mesozoic iron copper ore forming belt of Chi-na, Which is Clasely related to tnagmatic activities and extenils along the continental deep fault or rift, as we call theYangtze magmatic rock belt. The along-Yangtze Tiver area of Anhui, Lying on the middle Section of the belt is rep-resented by complete rock typos and clear structure appearances for study. |
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| Keywords: | Yangthe Magmatic rocks characteristics Anhui |
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