Narmada–Son lineament
E918311
The Narmada–Son lineament is a major east–west-trending tectonic feature in central India that marks a significant crustal boundary and influences regional seismicity, river courses, and basin development.
Statements (41)
| Predicate | Object |
|---|---|
| instanceOf |
crustal boundary
ⓘ
geological structure ⓘ tectonic lineament ⓘ |
| associatedWith |
Narmada River
NERFINISHED
ⓘ
Son River NERFINISHED ⓘ fault-controlled valleys ⓘ intraplate seismicity in central India ⓘ rift-related structures ⓘ |
| controls |
alignment of several river valleys
ⓘ
location of several sedimentary basins ⓘ structural configuration of central Indian basins ⓘ |
| country | India ⓘ |
| extendsFrom | western India ⓘ |
| extendsTo | eastern India ⓘ |
| geologicalAge | Precambrian origin (reactivated later) ⓘ |
| geophysicalSignature | crustal-scale lineament visible in geophysical data ⓘ |
| influences |
basin development
ⓘ
drainage pattern of central India ⓘ regional seismicity ⓘ river courses ⓘ |
| linkedTo |
differential uplift and subsidence in central India
ⓘ
formation of rift basins along its course ⓘ |
| locatedIn | central India ⓘ |
| marks |
boundary between different tectonic blocks
ⓘ
major crustal discontinuity ⓘ |
| namedAfter |
Narmada River
NERFINISHED
ⓘ
Son River NERFINISHED ⓘ |
| orientation | east–west ⓘ |
| partOf |
Indian shield
NERFINISHED
ⓘ
intraplate tectonic framework of India ⓘ |
| reactivatedDuring | Phanerozoic ⓘ |
| relatedTo | fault systems in central India ⓘ |
| relevance |
groundwater occurrence and movement
ⓘ
hydrocarbon exploration in central Indian basins ⓘ seismic hazard assessment in central India ⓘ |
| separates |
northern Indian crustal blocks
ⓘ
southern Indian crustal blocks ⓘ |
| studiedIn | Indian tectonics ⓘ |
| tectonicActivity | neotectonic movements ⓘ |
| trend | east–west ⓘ |
| typeOfBoundary | tectonic and crustal boundary ⓘ |
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.