packstone (Q41285): Difference between revisions
From geokb
(Created a new Item: Added initial named and identified rock item from Mindat) |
(Changed an Item: Updated rock class item with Geoscience Ontology GSRM subclass data) |
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| label / en | label / en | ||
packstone | |||
| description / en | description / en | ||
Carbonate sedimentary rock with discernible grain supported depositional texture, containing greater than 10 percent grains, and constituent particles are of intrabasinal origin; intergranular spaces are filled by matrix. | |||
| Property / instance of | |||
| Property / instance of: rock material / rank | |||
| Property / instance of: rock material / reference | |||
| Property / Mindat identifier | |||
| Property / Mindat identifier: 50886 / rank | |||
| Property / subclass of | |||
| Property / subclass of: biochemical and chemical sedimentary rock / rank | |||
Normal rank | |||
| Property / subclass of: biochemical and chemical sedimentary rock / reference | |||
| Property / subclass of | |||
| Property / subclass of: carbonate sedimentary rock / rank | |||
Normal rank | |||
| Property / subclass of: carbonate sedimentary rock / reference | |||
| Property / subclass of: carbonate sedimentary rock / reference | |||
reference statement: Hallsworth and Knox 1999 | |||
| Property / same as | |||
| Property / same as: https://mindat.org/min-50886.html / rank | |||
Normal rank | |||
| Property / same as | |||
| Property / same as: https://w3id.org/gso/rockmaterial/packstone / rank | |||
Normal rank | |||
Latest revision as of 17:10, 24 October 2023
Carbonate sedimentary rock with discernible grain supported depositional texture, containing greater than 10 percent grains, and constituent particles are of intrabasinal origin; intergranular spaces are filled by matrix.
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | packstone |
Carbonate sedimentary rock with discernible grain supported depositional texture, containing greater than 10 percent grains, and constituent particles are of intrabasinal origin; intergranular spaces are filled by matrix. |
Statements
2 references
Hallsworth and Knox 1999
