Consideration of Magnetic Particle Testing using Rotating Magnetic Field of Omnidirectional Crack in Three-dimensional Shape Portion and Evaluation of Flaw Detection Performance

Figure S1 showing locations of magnetic high-low anomalies that exhibit total gradient highs, numbered 1–3 as described in the text with: (A) simplified surface geology (colors as in Fig. 2), arrow marks an area near metavolcanic rock described as Triassic to Pennsylvanian? by Wilson et al. (2015); (B) reduced-to-pole magnetic field; and (C) total gradient and thick black lines delineate faults interpreted in this study and by Haeussler and Saltus (2011).<br>

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Supplemental Material: Three-dimensional shape and structure of the Susitna basin, south-central Alaska, from geophysical data

10.1130/geos.s.12218234.v1 ◽

2020 ◽

Author(s):

A.K. Shah

Keyword(s):

Magnetic Field ◽

Three Dimensional ◽

Geophysical Data ◽

Metavolcanic Rock ◽

South Central ◽

Total Gradient ◽

Dimensional Shape ◽

Surface Geology ◽

Three Dimensional Shape

Figure S1 showing locations of magnetic high-low anomalies that exhibit total gradient highs, numbered 1–3 as described in the text with: (A) simplified surface geology (colors as in Fig. 2), arrow marks an area near metavolcanic rock described as Triassic to Pennsylvanian? by Wilson et al. (2015); (B) reduced-to-pole magnetic field; and (C) total gradient and thick black lines delineate faults interpreted in this study and by Haeussler and Saltus (2011).<br>

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Supplemental Material: Three-dimensional shape and structure of the Susitna basin, south-central Alaska, from geophysical data

10.1130/geos.s.12218234 ◽

2020 ◽

Author(s):

A.K. Shah ◽

et al.

Keyword(s):

Magnetic Field ◽

Three Dimensional ◽

Geophysical Data ◽

Metavolcanic Rock ◽

South Central ◽

Total Gradient ◽

Dimensional Shape ◽

Surface Geology ◽

Three Dimensional Shape

Figure S1 showing locations of magnetic high-low anomalies that exhibit total gradient highs, numbered 1–3 as described in the text with: (A) simplified surface geology (colors as in Fig. 2), arrow marks an area near metavolcanic rock described as Triassic to Pennsylvanian? by Wilson et al. (2015); (B) reduced-to-pole magnetic field; and (C) total gradient and thick black lines delineate faults interpreted in this study and by Haeussler and Saltus (2011).<br>

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A Three-dimensional Shape Measurement Method Requiring only a Single Observation Image Based on Pattern Projection Technique

IEEJ Transactions on Electronics Information and Systems ◽

10.1541/ieejeiss.131.2224 ◽

2011 ◽

Vol 131 (12) ◽

pp. 2224-2225

Author(s):

Ke Sun ◽

Cunwei Lu

Keyword(s):

Measurement Method ◽

Three Dimensional ◽

Shape Measurement ◽

Projection Technique ◽

Single Observation ◽

Pattern Projection ◽

Dimensional Shape ◽

Three Dimensional Shape

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Four Dimensions of Diamond T: Combination Trade Marks of Colours And Shapes

Victoria University of Wellington Law Review ◽

10.26686/vuwlr.v37i4.5584 ◽

2006 ◽

Vol 37 (4) ◽

pp. 583

Author(s):

Michael McGowan

Keyword(s):

Three Dimensional ◽

Trade Mark ◽

Fourth Dimension ◽

Trade Marks ◽

Four Dimensions ◽

Trade Mark Law ◽

Dimensional Shape ◽

Three Dimensional Shape

This article examines the relatively new fields of colour and shape trade marks. It was initially feared by some academics that the new marks would encroach on the realms of patent and copyright. However, the traditional requirements of trade mark law, such as functionality and descriptiveness, have meant that trade marks in colour and shape are extremely hard to acquire if they do not have factual distinctiveness. As colour and shape trade marks have no special restrictions, it is proposed that the combination trade mark theory and analysis from the Diamond T case should be used as a way to make them more accessible. The combination analysis can be easily applied because every product has a three dimensional shape and a fourth dimension of colour.

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