Tipo de limites de placas tectônicas
Tipo de limites de placas tectônicas
Tipo de limites de placas tectônicas
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<strong>Tipo</strong> <strong>de</strong> <strong>limites</strong> <strong>de</strong><br />
<strong>placas</strong> tectônicas<br />
Pedro Wagner Gonçalves<br />
Departamento <strong>de</strong> Geociências Aplicadas<br />
ao Ensino<br />
Instituto <strong>de</strong> Geociências - UNICAMP<br />
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ipos <strong>de</strong> <strong>limites</strong> <strong>de</strong> <strong>placas</strong><br />
ansformante Divergente Subducção<br />
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imite divergente ou dorsal<br />
Usualmente dá origem a cordilheira meso-oceânica<br />
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ício do processo <strong>de</strong> separaçã<br />
e <strong>placas</strong><br />
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imites construtivos e<br />
estrutivos<br />
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imite <strong>de</strong> subducção: : oceano-<br />
ceano (formação <strong>de</strong> arco<br />
ulcânico)<br />
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imite <strong>de</strong> subducção:<br />
ontinente-oceano<br />
oceano<br />
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alha transformante<br />
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alha transformante (limite<br />
onservativo)<br />
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dinâmica <strong>de</strong> tectônica <strong>de</strong> <strong>placas</strong> e a formaçã<br />
s continentes<br />
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dia: explicação da colisão<br />
e duas <strong>placas</strong> continentais<br />
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Fig. 2.1
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Fig. 2.15
Fig. 2.15<br />
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Fig. 2.15<br />
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Fig. 2.15
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Fig. 2.15
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Fig. 2.1
Fig. 2.15<br />
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Fig. 2.15<br />
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Fig. 2.15