cataclasite series (Q161266): Difference between revisions
From geokb
(Created a new Item: Added new rock class item from Geoscience Ontology GSRM data) |
(Changed an Item: Updated rock class item with Geoscience Ontology GSRM subclass data) |
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| Property / subclass of | |||
| Property / subclass of: composite genesis rock / rank | |||
Normal rank | |||
| Property / subclass of: composite genesis rock / reference | |||
| Property / subclass of: composite genesis rock / reference | |||
reference statement: Sibson, 1977 | |||
| Property / subclass of: composite genesis rock / reference | |||
reference statement: Scholz, 1990 | |||
| Property / subclass of: composite genesis rock / reference | |||
reference statement: Snoke and Tullis, 1998 | |||
| Property / subclass of: composite genesis rock / reference | |||
reference statement: Barker, 1998 Appendix II | |||
| Property / subclass of: composite genesis rock / reference | |||
| Property / subclass of | |||
| Property / subclass of: fault related material / rank | |||
Normal rank | |||
| Property / subclass of: fault related material / reference | |||
| Property / subclass of: fault related material / reference | |||
reference statement: Sibson, 1977 | |||
| Property / subclass of: fault related material / reference | |||
reference statement: Scholz, 1990 | |||
| Property / subclass of: fault related material / reference | |||
reference statement: Snoke and Tullis, 1998 | |||
| Property / subclass of: fault related material / reference | |||
reference statement: Barker, 1998 Appendix II | |||
| Property / subclass of: fault related material / reference | |||
Latest revision as of 17:09, 24 October 2023
Fault-related rock that maintained primary cohesion during deformation, with matrix comprising greater than 10 percent of rock mass; matrix is fine-grained material formed through grain size reduction by fracture as opposed to crystal plastic process
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | cataclasite series |
Fault-related rock that maintained primary cohesion during deformation, with matrix comprising greater than 10 percent of rock mass; matrix is fine-grained material formed through grain size reduction by fracture as opposed to crystal plastic process |
Statements
6 references
Sibson, 1977
Scholz, 1990
Snoke and Tullis, 1998
Barker, 1998 Appendix II
6 references
Sibson, 1977
Scholz, 1990
Snoke and Tullis, 1998
Barker, 1998 Appendix II
