孤立台地相

位于大洋之中,离开陆架常有数十到数百千米,常位于断陷陆壳或过渡壳之上,并被深水所包围。台地外缘为环礁带,内缘为骨屑灰岩或鲕粒灰岩,内部为团粒灰岩和泥晶灰岩。台地边缘前斜坡为碎石堆、滑塌和重力流碳酸盐沉积,盆地为远源钙屑浊积岩、浮游生物灰岩及泥晶灰岩。

Concept & Semantic
  26

Alias

孤立台地相

Contributor

contributed at 2011-09-27

Classification(s)

Earth System(in Chinese)Sedimentology and sedimentary petrology

Detailed Description

English
Name isolated platform facies
Chinese
Name 孤立台地相
Description 位于大洋之中,离开陆架常有数十到数百千米,常位于断陷陆壳或过渡壳之上,并被深水所包围。台地外缘为环礁带,内缘为骨屑灰岩或鲕粒灰岩,内部为团粒灰岩和泥晶灰岩。台地边缘前斜坡为碎石堆、滑塌和重力流碳酸盐沉积,盆地为远源钙屑浊积岩、浮游生物灰岩及泥晶灰岩。

How to Cite

NNU_Group (2011). 孤立台地相, Concept & Semantic, OpenGMS, https://geomodeling.njnu.edu.cn/repository/concept/6ac595cc-dc53-4e7f-8e9d-3d9097f88b7f
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Contributor

contributed at 2011-09-27

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