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Data · dataset · 2025

Crustal anisotropy in the source area of the 2017 Puebla-Morelos Earthquake

Listed in Teesside University Research Data Repository

The anisotropic data from this repository correspond to the parameters of fast polarization and normalized delay time obtained using the Shear Wave Splitting methodology from seismic events that occurred in the Puebla-Morelos area.

Description

These are separated according to each figure in the article titled Spatiotemporal variation and structural characterization of crustal anisotropy in the source area of the 2017 Puebla-Morelos Earthquake.

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Where it is published

Catalogue records · 1

Topics

Provenance · 1 source records, 6 field assertions
SourceKeyLast seenRaw
Teesside University Research Data Repositoryoai:data.mendeley.com/cxtd7ypy5c.115 h agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · researchdata tees ac ukconnector:researchdata_tees_ac_uk@1.0.0
concepts[field].local:field:earth-environmentalmapping · researchdata tees ac ukconnector:researchdata_tees_ac_uk@1.0.0
descriptionsource · researchdata tees ac ukconnector:researchdata_tees_ac_uk@1.0.0/metadata/dc/description
licensesource · researchdata tees ac ukconnector:researchdata_tees_ac_uk@1.0.0/metadata/dc/rights
publication_datesource · researchdata tees ac ukconnector:researchdata_tees_ac_uk@1.0.0
titlesource · researchdata tees ac ukconnector:researchdata_tees_ac_uk@1.0.0/metadata/dc/title