What is this layer?
The distribution of clastic sedimentary rocks in Western Australia. Clastic sedimentary rocks may form in a basinal environment. Basins are considered to be potential source areas for the circulation of manganese-rich fluids and the early concentration of manganese in carbonate-rich rocks.
Legend
| Legend | Description |
|---|---|
| Clastic sedimentary rocks dominant | Clastic sedimentary rocks are considered to be a dominant lithology within the polygon. There is a high probability of observing clastic sedimentary rocks in these areas |
| Clastic sedimentary rocks minor | Clastic sedimentary rocks are considered to be a minor lithology within the polygon. There is a low probability of observing clastic sedimentary rocks in these areas |
Filtered with
| Operation | Query |
|---|---|
| Metasedimentary siliciclastic, metasedimentary siliciclastic: pelite, metasedimentary siliciclastic: psammite and pelite; interlayered, metasedimentary siliciclastic: psephite, metasedimentary siliciclastic: semipelite, metasedimentary siliciclastic: semipsephite, sedimentary siliciclastic | LOWER (ROCKTYPE1) LIKE LOWER ('%siliciclastic%') OR LOWER (ROCKTYPE2) LIKE LOWER ('%siliciclastic%') |
Model logic and recipe
|
Operation |
Expression |
Operation |
Expression |
Operation |
Expression |
Operation |
|---|---|---|---|---|---|---|
|
Select |
LOWER (ROCKTYPE1) LIKE LOWER ('%siliciclastic%') OR LOWER (ROCKTYPE2) LIKE LOWER ('%siliciclastic%') |
Select1 |
LOWER (ROCKTYPE1) LIKE LOWER ('%siliciclastic%') |
Calculate Field |
‘Clastic sedimentary dominant’ |
Merge |
|
|
|
Select2 |
LOWER (ROCKTYPE2) LIKE LOWER ('%siliciclastic%') |
Calculate Field (2) |
‘Clastic sedimentary minor’ |
