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Commit d5cc68ae authored by Powers, Peter M.'s avatar Powers, Peter M.
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Merge branch 'cli-continued' into 'main'

Dependency updates

See merge request !573
parents f2f289c0 49830bd6
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2 merge requests!577Production Release | nshmp-haz,!573Dependency updates
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with 24 additions and 19 deletions
......@@ -25,4 +25,5 @@ libs
# Node
node_modules
package.json
package-lock.json
......@@ -29,7 +29,7 @@
plugins {
id "application"
id "com.diffplug.gradle.spotless" version "${spotlessVersion}"
id "com.diffplug.spotless" version "${spotlessVersion}"
id "com.github.johnrengelman.shadow" version "${shadowVersion}"
id "com.github.node-gradle.node" version "${nodeVersion}"
id "com.github.spotbugs" version "${spotbugsVersion}"
......@@ -60,6 +60,10 @@ jacoco {
test {
useJUnitPlatform()
filter {
excludeTestsMatching "gov.usgs.earthquake.nshmp.model.NshmTestsLarge"
}
}
jacocoTestReport {
......
......@@ -37,7 +37,7 @@ for rupture geometry. Truncated Gutenberg-Richter MFDs are used to model grid so
magnitudes and rates with logic trees of varying a-value, b-value and maximum magnitude. For grid
sources the relative rate at each grid node is defined using a spatial PDF (see notes on
spatial PDFs, [below](#spatial-pdfs)). When realizing each source the spatial PDF value is scaled
by each regional rate in a rate-tree.
by each regional rate in a required `rate-tree`.
Grid sources are represented in a model using a logic tree with a `rupture-sets.json` defining the
ruptures on each branch. Because gridded seismicity models may be governed by regionally
......
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