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      <title>Trabalho sobre Teoria Tectónicas de Placas, dobras e falhas by Daniel Santos</title>
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      <language>en-us</language>
      <pubDate>2018-02-15 19:07:54 UTC</pubDate>
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         <title>Teoria da téctonica de placas</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/233014402</link>
         <description><![CDATA[<div>Após a 2ª Guerra Mundial na década de 60 do século XX, numerosos cientistas juntaram-se para saber mais sobre os fundos ocêanicos e a estrutura interna da Terra.<br><br>No final do século foi proposta a teoria da téctonica de placas</div><div><br><br></div>]]></description>
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         <pubDate>2018-02-19 18:25:10 UTC</pubDate>
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         <title>Dobras</title>
         <author>gabiman6969</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/233026591</link>
         <description><![CDATA[<div>Deformação que ocorre nas rochas e que resulta do arqueamento de camadas rochosas, inicialmente planas, com comportamento dúctil, pela ação de tensões compressivas.<br>As dobras formam-se no interior da crusta ou do manto de forma lenta e gradual, emergindo à superfície devido aos movimentos tectónicos e à erosão.<br><br></div>]]></description>
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         <pubDate>2018-02-19 19:05:16 UTC</pubDate>
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         <title>Tipos de forças tectónicas</title>
         <author>daniel_santos1901</author>
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         <pubDate>2018-02-19 19:06:48 UTC</pubDate>
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         <title>Forças compressivas</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/233028203</link>
         <description><![CDATA[<div>Provocam a compreensão dos materiais rochosos. Reduzem o volume da rocha ou aproximam os blocos rochosos.</div>]]></description>
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         <pubDate>2018-02-19 19:10:07 UTC</pubDate>
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         <title>Forças distensivas</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/233028830</link>
         <description><![CDATA[<div>Provocam a distensão dos materias rochosos. Alongam a rocha ou afastam os blocos rochosos</div>]]></description>
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         <pubDate>2018-02-19 19:12:18 UTC</pubDate>
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         <title>Forças de cisalhamento</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/233032075</link>
         <description><![CDATA[<div>Provocam movimentos paralelos das rochas em sentidos opostos.</div>]]></description>
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         <pubDate>2018-02-19 19:22:28 UTC</pubDate>
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         <title>Falhas</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/233942126</link>
         <description><![CDATA[<div>As rochas quando sujeitas a forças tectónicas e ultrapassam o seu limite de resistência à rutura, as rochas fraturam. A este comportamento dá-se o nome de <strong>comportamento frágil.<br></strong>Se os blocos de rochas se deslocarem em relação ao outro formou-se uma <strong>falha.</strong></div>]]></description>
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         <pubDate>2018-02-21 19:21:12 UTC</pubDate>
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         <title>Tipos de falhas</title>
         <author>daniel_santos1901</author>
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         <pubDate>2018-02-26 18:42:39 UTC</pubDate>
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         <title>Falhas normais</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/235551997</link>
         <description><![CDATA[<div><figure class="attachment attachment--preview"><img src="https://scontent.flis6-1.fna.fbcdn.net/v/t34.0-12/28236070_1321637607936566_1963460729_n.png?oh=05340da10345e81228f5ddc300b8729e&amp;oe=5A96132F" width="204" height="114"><figcaption class="attachment__caption"></figcaption></figure>o </div><div><strong>teto</strong> vai para baixo e o <strong>muro</strong> para cima</div>]]></description>
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         <pubDate>2018-02-26 18:44:21 UTC</pubDate>
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         <title>Falhas inversas</title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/235553926</link>
         <description><![CDATA[<div><figure class="attachment attachment--preview"><img src="https://scontent.flis6-1.fna.fbcdn.net/v/t34.0-12/28235972_1321636887936638_199863762_n.png?oh=bfd7f7e70bbc8418df44e96d769e56f9&amp;oe=5A9628EF" width="186" height="105"><figcaption class="attachment__caption"></figcaption></figure>o <strong>teto </strong>vai para cima e o <strong>muro</strong> vai para baixo</div>]]></description>
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         <pubDate>2018-02-26 18:46:42 UTC</pubDate>
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         <title></title>
         <author>daniel_santos1901</author>
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         <description><![CDATA[￼]]></description>
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         <pubDate>2018-02-26 18:51:49 UTC</pubDate>
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         <title>Falhas de desligamento </title>
         <author>daniel_santos1901</author>
         <link>https://padlet.com/daniel_santos1901/bw6h96jhkdbu/wish/235560348</link>
         <description><![CDATA[<div><figure class="attachment attachment--preview"><img src="https://scontent.flis6-1.fna.fbcdn.net/v/t34.0-12/28459128_1326120530821607_491667767_n.png?oh=cb7f1d4ec3d548539737ce4ac93b9391&amp;oe=5A961B35" width="222" height="151"><figcaption class="attachment__caption"></figcaption></figure>não existe teto nem muro apenas um dos blocos rochosos se movimenta em relação ao outro</div>]]></description>
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         <pubDate>2018-02-26 18:55:37 UTC</pubDate>
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         <title>https://pt.slideshare.net/treis/teoria-da-tectnica-de-placas-3580742</title>
         <author>daniel_santos1901</author>
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         <pubDate>2018-02-26 19:11:32 UTC</pubDate>
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         <title>Trabalho realizado por Daniel Pinto e Gabriel Hauer.</title>
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         <pubDate>2018-02-26 19:24:39 UTC</pubDate>
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