Difference between revisions of "Translations:Dictionary:Fig P-5/2/en"

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Message definition (Dictionary:Fig P-5)
FIG. P-5. (<b>a</b>) <b>Plate-tectonic model</b>. A=rift zone where plates ''P''<sub>1</sub> and ''P''<sub>4</sub> are moving apart (such as the Mid-Atlantic Ridge) where new crust is being created. ''C''=ocean trench resulting from overriding of plate ''P''<sub>3</sub> over ''P''<sub>1</sub> (or ''P''<sub>2</sub> over ''P''<sub>4</sub>); ''B''=Benioff-Wadati zone of earthquakes dipping along the contact of plates ''P''<sub>1</sub> and ''P''<sub>2</sub> which are colliding. ''T''=transform faults where plates are sliding by each other. (After Isaacs et al., 1968.) (<b>b</b>) There are three kinds of plate boundaries. The junction of three plates constitutes a ''[[Special:MyLanguage/Dictionary:triple_junction|triple junction]]'' (q.v.); See also Fig. T-16.
TranslationFIG. P-5. (<b>a</b>) <b>Plate-tectonic model</b>. A=rift zone where plates ''P''<sub>1</sub> and ''P''<sub>4</sub> are moving apart (such as the Mid-Atlantic Ridge) where new crust is being created. ''C''=ocean trench resulting from overriding of plate ''P''<sub>3</sub> over ''P''<sub>1</sub> (or ''P''<sub>2</sub> over ''P''<sub>4</sub>); ''B''=Benioff-Wadati zone of earthquakes dipping along the contact of plates ''P''<sub>1</sub> and ''P''<sub>2</sub> which are colliding. ''T''=transform faults where plates are sliding by each other. (After Isaacs et al., 1968.) (<b>b</b>) There are three kinds of plate boundaries. The junction of three plates constitutes a ''[[Special:MyLanguage/Dictionary:triple_junction|triple junction]]'' (q.v.); See also Fig. T-16.

FIG. P-5. (a) Plate-tectonic model. A=rift zone where plates P1 and P4 are moving apart (such as the Mid-Atlantic Ridge) where new crust is being created. C=ocean trench resulting from overriding of plate P3 over P1 (or P2 over P4); B=Benioff-Wadati zone of earthquakes dipping along the contact of plates P1 and P2 which are colliding. T=transform faults where plates are sliding by each other. (After Isaacs et al., 1968.) (b) There are three kinds of plate boundaries. The junction of three plates constitutes a triple junction (q.v.); See also Fig. T-16.