放射虫岩 Radiolarite
(重定向自Radiolarian chert)
放射虫岩是硅质岩的一种,硬度较高、粒度较细、与燧石相似,主要由放射虫死亡后的残骸构成。放射虫岩这一名词也应用于已固结的放射虫软泥。未固结的放射虫岩被称为放射虫土。放射虫燧石是层理发育,微晶的放射虫岩,硅质胶结或硅质基质的一种放射虫岩。
单词 | Radiolarian chert |
释义 |
Radiolarian chert
中文百科
放射虫岩 Radiolarite(重定向自Radiolarian chert)
放射虫岩是硅质岩的一种,硬度较高、粒度较细、与燧石相似,主要由放射虫死亡后的残骸构成。放射虫岩这一名词也应用于已固结的放射虫软泥。未固结的放射虫岩被称为放射虫土。放射虫燧石是层理发育,微晶的放射虫岩,硅质胶结或硅质基质的一种放射虫岩。
英语百科
Radiolarite 放射虫岩(重定向自Radiolarian chert)
![]() ![]() ![]() ![]() Radiolarite is a siliceous, comparatively hard, fine-grained, chert-like, and homogeneous sedimentary rock that is composed predominantly of the microscopic remains of radiolarians. This term is also used for indurated radiolarian oozes and sometimes as a synonym of radiolarian earth. However, radiolarian earth is typically regarded by Earth scientists to be the unconsolidated equivalent of a radiolarite. A radiolarian chert is well-bedded, microcrystalline radiolarite that has a well-developed siliceous cement or groundmass. |
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