| 混积岩的分类和成因 |
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| 引用本文： | 张雄华.混积岩的分类和成因[J].地质科技情报,2000,19(4):31-34. |
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| 作者姓名： | 张雄华 |
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| 作者单位： | 中国地质大学地球科学学院湖北武汉 430074 |
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| 基金项目： | 江西省“修水县幅、三都幅 1∶ 5 0 0 0 0区调项目”，湖南省“四都坪幅、马底驿幅 1∶ 5 0 0 0 0区调项目” |
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| 摘 要： | 对在混合作用的特征者了系统的阐述和讨论，混积岩是陆源碎屑和碳酸盐颗粒及灰泥混合在一起的沉积岩，属曲型陆源碎屑岩和碳酸盐岩之间的过渡类型，据其成分可分为４类，陆源碎屑和碳酸盐颗粒，灰泥的混合作用从成因上分为５种类型，副件突变沉积混合，相缘渐变沉积混合，原地沉积混合，侵蚀再沉积混合，岩溶穿插再沉积混合。
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| 关 键 词： | 混积岩 沉积岩 陆源碎屑 碳酸盐 灰泥 成因 分类 |
| 文章编号： | 1000-7849(2000)04-0031-04 |
| 修稿时间： | 2000年6月2日 |
CLASSIFICATION AND ORIGIN OF MIXOSEDIMENTITE |
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| Zhang Xionghua.CLASSIFICATION AND ORIGIN OF MIXOSEDIMENTITE[J].Geological Science and Technology Information,2000,19(4):31-34. |
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| Authors: | Zhang Xionghua |
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| Abstract: | Mixosedimentite is formed by the mixing of terrigenous clastics,carbonate clastics and mud,belonging to the intermediate between typical silicilastic and carbonate sediments.It can be classfied into four main kinds according to its composition.While the mixing of siliciclastic and carbonate sediments can be divided into five kinds according to their origin:mixed by sudden event; by gardual facies change;mixed in situ; by erosion; by palaeokarst.The characteristics of the mixing are described and discussed systematically in the paper. |
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| Keywords: | mixosedimentite classification orig( |
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