潮间带相
位于平均高潮线与平均低潮线之间的区域的沉积，宽数万米。潮坪主要由泥晶石灰岩、球粒石灰岩组成，常发生白云石化。含腹足类、有孔虫及藻类叠层石。具生物扰动构造、生物潜穴及水平层理，局部见小型交错层理、干裂等。
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Alias
Contributor
contributed at 2011-09-27
Classification(s)
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Earth System(in Chinese) Sedimentology and sedimentary petrology
Detailed Description
| English |
|---|
| Name | intertidal zone facies |
| Chinese |
|---|
| Name | 潮间带相 |
| Description | 位于平均高潮线与平均低潮线之间的区域的沉积，宽数万米。潮坪主要由泥晶石灰岩、球粒石灰岩组成，常发生白云石化。含腹足类、有孔虫及藻类叠层石。具生物扰动构造、生物潜穴及水平层理，局部见小型交错层理、干裂等。 |
How to Cite
NNU_Group (2011). 潮间带相, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/e8cc1e33-8662-46e6-b6fd-1aa257c568b4
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