协同沉积
由两种或两种以上运动方式的水流协同作用形成的次生碳酸钙沉积物。常见的协同方式及典型沉积物有：①滴水流水沉积，如堆状石笋、片状石钟乳、外层被流石覆盖的大型石笋和石柱等；②滴水飞溅水沉积，如棕榈石笋；③滴水池水沉积，如蚀膜晶锥、滴坑穴珠；④滴水池水流水沉积，如云盆；⑤滴水非重力水沉积，如乳房状石钟乳、石瘤、珠状石钟乳等。其形成多在非重力水向重力水过渡的临界状态下，所以常与鹅管共生。
46
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Contributor
contributed at 2011-10-12
Classification(s)
●
Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | synergetic deposits |
| Chinese |
|---|
| Name | 协同沉积 |
| Description | 由两种或两种以上运动方式的水流协同作用形成的次生碳酸钙沉积物。常见的协同方式及典型沉积物有：①滴水流水沉积，如堆状石笋、片状石钟乳、外层被流石覆盖的大型石笋和石柱等；②滴水飞溅水沉积，如棕榈石笋；③滴水池水沉积，如蚀膜晶锥、滴坑穴珠；④滴水池水流水沉积，如云盆；⑤滴水非重力水沉积，如乳房状石钟乳、石瘤、珠状石钟乳等。其形成多在非重力水向重力水过渡的临界状态下，所以常与鹅管共生。 |
How to Cite
NNU_Group (2011). 协同沉积, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/20d19a4f-2fe7-4d6f-bfe2-315f6a52b53d
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