层间砾岩
又称层内砾岩、同生砾岩(syngenetic conglomerate)。一种位于某地层内部的砾岩。它与上下地层之间为连续沉积，无沉积间断。这种砾岩的碎屑与基质充填物是由于沉积不久的或只有部分固结的沉积物，在准同生期破碎成砾石或角砾碎屑堆积而成的，如滑塌角砾岩，生物礁的礁前塌积岩，中国北方寒武系中的竹叶状灰岩属之。
Classification(s)
●
Geographic semantic resource library Earth System(in Chinese) Sedimentology and sedimentary petrology
{{htmlJSON.DetailedDescription}}
| English |
|---|
| Name | intraformational conglomerate |
| Chinese |
|---|
| Name | 层间砾岩 |
| Description | 又称层内砾岩、同生砾岩(syngenetic conglomerate)。一种位于某地层内部的砾岩。它与上下地层之间为连续沉积，无沉积间断。这种砾岩的碎屑与基质充填物是由于沉积不久的或只有部分固结的沉积物，在准同生期破碎成砾石或角砾碎屑堆积而成的，如滑塌角砾岩，生物礁的礁前塌积岩，中国北方寒武系中的竹叶状灰岩属之。 |
{{htmlJSON.HowtoCite}}
NNU_Group (2011). 层间砾岩, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/b94e7664-9c6c-439a-b745-faea222a0696
{{htmlJSON.Copy}}
Copyright and Disclaimer
All copyrights of a material (model, data, article, etc.) in the OpenGMS fully belong to its author/developer/designer (or any other wording about the owner). The OpenGMS takes every care to avoid copyright infringement, contributor(s) should carefully employ materials from other sources and give proper citations.
