arcmap gis software v.10.3 (Esri inc)
Structured Review
Arcmap Gis Software V.10.3, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcmap+v%2E10%2E3+software/arcgis+10+2/pm39441233-106-15-21
Average 90 stars, based on 1 article reviews
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Generated:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with Software:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with Northern Blot:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with Migration:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with Activity Assay:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with Western Blot:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with Derivative Assay:Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: VMG has distinctive La/Yb ( C ) and Dy/Yb ( D ) values, i.e. a completely different signature between VMG magmas and VH magmas. ( E ) Distribution (perpendicular distance (km) and normalised along-strike of the LOFZ) of stratovolcanoes and monogenetic cones from 41.5° to 47.5° S based on our mapping. ( F , G ) DEMs and mapping from the VMG, showing the 5 km by 4 km caldera, the young partially collapsed cone, the rock avalanche deposits (QRa), Quaternary alluvium (Qal), and the location of the main trace of the LOFZ that cuts this cone and displaces the rock avalanche deposit (likely triggered by a LOFZ earthquake/rupture) northward (i.e. dextrally) by ~ 170 ± 20 m. Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base image was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Field and helicopter photos from this site are shown in Fig. . Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Base hillshade was generated with Article Title: Slip rates along the narrow Magallanes Fault System, Tierra Del Fuego Region, Patagonia Article Snippet: Topographic profiles were generated with |
