bio rad cfx manager software version 3 0 Search Results


vrml-view version 3.0  (Kongsberg Maritime Contros GmbH)
90
Kongsberg Maritime Contros GmbH vrml-view version 3.0
Vrml View Version 3.0, supplied by Kongsberg Maritime Contros GmbH, 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/bio+rad+cfx+manager+software+version+3+0/vrml+view+version+3+0/pmc02893942-75-58-65
Average 90 stars, based on 1 article reviews
vrml-view version 3.0 - by Bioz Stars, 2026-09
90/100 stars
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sound forge version 3.0d  (Sony)
90
Sony sound forge version 3.0d
Sound Forge Version 3.0d, supplied by Sony, 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/bio+rad+cfx+manager+software+version+3+0/sound+forge+version+3+0d/10__1139_slash_cjz___2016___0166-61-17-21
Average 90 stars, based on 1 article reviews
sound forge version 3.0d - by Bioz Stars, 2026-09
90/100 stars
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georeferenced in arcgis pro version 3.0.36056  (Esri inc)
90
Esri inc georeferenced in arcgis pro version 3.0.36056
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Georeferenced In Arcgis Pro Version 3.0.36056, 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/bio+rad+cfx+manager+software+version+3+0/georeferenced+in+arcgis+pro+version+3+0+36056/pmc12069532-123-32-37
Average 90 stars, based on 1 article reviews
georeferenced in arcgis pro version 3.0.36056 - by Bioz Stars, 2026-09
90/100 stars
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genechip dna analysis software  (Thermo Fisher)
99
Thermo Fisher genechip dna analysis software
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Genechip Dna Analysis Software, supplied by Thermo Fisher, used in various techniques. Bioz Stars score: 99/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/bio+rad+cfx+manager+software+version+3+0/DNA/pmc03701888-66-5-11
Average 99 stars, based on 1 article reviews
genechip dna analysis software - by Bioz Stars, 2026-09
99/100 stars
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multi gauge software version 3.0  (FUJIFILM)
90
FUJIFILM multi gauge software version 3.0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Multi Gauge Software Version 3.0, supplied by FUJIFILM, 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/bio+rad+cfx+manager+software+version+3+0/multi+gauge+software/pm34033829-119-5-10
Average 90 stars, based on 1 article reviews
multi gauge software version 3.0 - by Bioz Stars, 2026-09
90/100 stars
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grafit version 3.0 program  (ERITHACUS SOFTWARE LIMITED)
90
ERITHACUS SOFTWARE LIMITED grafit version 3.0 program
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Grafit Version 3.0 Program, supplied by ERITHACUS SOFTWARE LIMITED, 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/bio+rad+cfx+manager+software+version+3+0/grafit+5/10__1042_slash_bj20020840-43-12-20
Average 90 stars, based on 1 article reviews
grafit version 3.0 program - by Bioz Stars, 2026-09
90/100 stars
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arcgis pro  (Esri inc)
90
Esri inc arcgis pro
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro, 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/bio+rad+cfx+manager+software+version+3+0/arcgis+pro/10__7589_slash_jwd___d___22___00148-30-15-19
Average 90 stars, based on 1 article reviews
arcgis pro - by Bioz Stars, 2026-09
90/100 stars
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statistical software statxact version 3.0  (Cytel Software)
90
Cytel Software statistical software statxact version 3.0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Statistical Software Statxact Version 3.0, supplied by Cytel Software, 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/bio+rad+cfx+manager+software+version+3+0/statxact+software/pm14744843-50-9-14
Average 90 stars, based on 1 article reviews
statistical software statxact version 3.0 - by Bioz Stars, 2026-09
90/100 stars
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sarah nexus (version 3.0.0  (Lhasa Ltd)
90
Lhasa Ltd sarah nexus (version 3.0.0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Sarah Nexus (Version 3.0.0, supplied by Lhasa Ltd, 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/bio+rad+cfx+manager+software+version+3+0/sarah+nexus/pmc09330180-119-22-30
Average 90 stars, based on 1 article reviews
sarah nexus (version 3.0.0 - by Bioz Stars, 2026-09
90/100 stars
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empiria studio software version 3 0  (LI-COR)
98
LI-COR empiria studio software version 3 0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Empiria Studio Software Version 3 0, supplied by LI-COR, used in various techniques. Bioz Stars score: 98/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/bio+rad+cfx+manager+software+version+3+0/EMPIRIA+STUDIO+SOFTWARE+LICENSE/10__3390_slash_ijms26062583-300-5-10
Average 98 stars, based on 1 article reviews
empiria studio software version 3 0 - by Bioz Stars, 2026-09
98/100 stars
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cobra toolbox version 3 0 0  (MathWorks Inc)
96
MathWorks Inc cobra toolbox version 3 0 0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Cobra Toolbox Version 3 0 0, supplied by MathWorks Inc, used in various techniques. Bioz Stars score: 96/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/bio+rad+cfx+manager+software+version+3+0/Partial+Differential+Equation+Toolbox/bio_rxiv__2023__09__13__557398-204-0-9
Average 96 stars, based on 1 article reviews
cobra toolbox version 3 0 0 - by Bioz Stars, 2026-09
96/100 stars
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file conversion tool version 3.0  (MassMatrix Inc)
90
MassMatrix Inc file conversion tool version 3.0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
File Conversion Tool Version 3.0, supplied by MassMatrix 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/bio+rad+cfx+manager+software+version+3+0/file+conversion+tool/10__1074_slash_mcp__m113__027607-102-1-0
Average 90 stars, based on 1 article reviews
file conversion tool version 3.0 - by Bioz Stars, 2026-09
90/100 stars
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Image Search Results


( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in ArcGIS Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).

Journal: Scientific Reports

Article Title: Tomographic and volcanotectonic control on the 2021–2023 Fagradalsfjall eruptions, Iceland

doi: 10.1038/s41598-025-95169-6

Figure Lengend Snippet: ( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in ArcGIS Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).

Article Snippet: The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in ArcGIS Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).

Techniques: Tomography, Generated