| 碳酸盐台地高水位溢流沉积研究 |
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| 引用本文： | 刘贻军,邹艳荣.碳酸盐台地高水位溢流沉积研究[J].黑龙江科技学院学报,1998(2). |
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| 作者姓名： | 刘贻军 邹艳荣 |
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| 作者单位： | 中国地质大学 |
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| 摘 要： | 碳酸盐台地高水位溢流是指在海平面高水位期，台地沉积物被搬运到斜坡及较深水盆地中沉积下来所形成的沉积体。一般发育在镶边陆架型台地或平顶台地低纬度暖水区，它的形成受台地类型、台地斜坡坡度、海平面变化幅度等要素的制约。
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| 关 键 词： | 碳酸盐台地 高水位溢流 沉积特征 制约要素 |
Depositional Characteristics of Highstand Shedding on Carbonate Platforms |
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| Liu Yijun,Zou Yanrong.Depositional Characteristics of Highstand Shedding on Carbonate Platforms[J].Journal of Heilongjiang Institute of Science and Technology,1998(2). |
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| Authors: | Liu Yijun Zou Yanrong |
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| Institution: | Liu Yijun;Zou Yanrong (China University of Geosciences) (Mineral Resouces Development Dept.) |
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| Abstract: | The term "highstand shedding of carbonate platforms" means that carbonate plat forms shed most their sediments into the slopes or the formed sediments deposit into the deeper basins. Generally speaking, highstand sheddings Well develop in rimmed carbonate plat forms or top carbonate platforms with lower latitude and warm sea water settins, but its forming is restrained by the types of warm platform, the slope angles and the amplitude of sea level changes. |
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| Keywords: | carbonate platform highstand shedding depositional characteristics controlling factors |
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